<?xml version="1.0" encoding="UTF-8"?>
<metadata>
    <idinfo>
        <citation>
            <citeinfo>
                <origin>Jaime A. Hirtz, ORCID: 0000-0002-6701-0137</origin>
                <origin>Joseph P. Colgan, ORCID: 0000-0001-6671-1436</origin>
                <origin>Bryant W. Platt, ORCID: 0000-0001-6389-9015</origin>
                <origin>Samuel A. Johnstone, ORCID: 0000-0002-3945-2499</origin>
                <origin>Warren P. Roe, ORCID: 0000-0001-9667-1906</origin>
                <pubdate>20250601</pubdate>
                <title>Cooperative National Geologic Map: Precambrian geology</title>
                <geoform>vector digital data</geoform>
                <onlink>https://doi.org/10.5066/P13TSV2J</onlink>
                <lworkcit>
                    <citeinfo>
                        <origin>Samuel A. Johnstone, ORCID: 0000-0002-3945-2499</origin>
                        <origin>Joseph P. Colgan, ORCID: 0000-0001-6671-1436</origin>
                        <origin>Warren P. Roe, ORCID: 0000-0001-9667-1906</origin>
                        <pubdate>20250601</pubdate>
                        <title>A synthesis engine for constructing geologic maps of the United
                            States</title>
                        <edition>1.0</edition>
                        <geoform>publication</geoform>
                        <serinfo>
                            <sername>U.S. Geological Survey Data Series</sername>
                            <issue>1210</issue>
                        </serinfo>
                        <onlink>https://doi.org/10.3133/dr1210</onlink>
                    </citeinfo>
                </lworkcit>
            </citeinfo>
        </citation>
        <descript>
            <abstract>The USGS National Cooperative Geologic Mapping Program (NCGMP) was directed by
                Congress to create a new geologic map of the United States” by “bring[ing] together
                detailed national and continental-resolution 2D and 3D information produced
                throughout the Survey and by federal and state partners” (House Report 116-100). To
                fulfill this goal, the NCGMP created a map synthesis engine (Johnstone and others,
                2025) based on the Geologic Map Schema (GeMS) standard (NCGMP, 2020) and used it to
                bring together source geologic maps originally published by the USGS and State
                Geological Surveys. This thematic map layer was derived from this database using
                procedures described by Johnstone and others (2025) and is intended to serve as a
                legible national map of the nation; while it retains full descriptions of geologic
                units from source materials it does not include the full search functionality
                (described in Johnstone and others, 2025) that is facilitated by a true relational
                database.
                The Precambrian Geology layer depicts all Precambrian rocks in the United
                States, inclusive of map units with minimum ages younger than Precambrian, such as
                the “Paleozoic to Precambrian” units shown on some older maps. The map was
                composited from all geologic maps that show Precambrian rocks, including where they
                are mostly buried beneath Phanerozoic sedimentary rocks and inferred from boreholes
                and geophysical data. In areas covered by maps of both Precambrian outcrops and
                buried Precambrian basement, the outcropping Precambrian units are preserved instead
                of the more generalized buried units. Due to the great disparity in scale and degree
                of interpretation between outcrop maps and subsurface maps, the Precambrian layer is
                highly discontinuous along map boundaries. Phanerizoic rocks are included in the
                map, subdivided into stratified rocks vs. igneous and metamorphic rocks. The map is
                structured as a single GeMS database with three additional tables (also described in
                Johnstone and others, 2025); a Source_DescriptionOfMapunits table preserves all
                source inputs, a synthesis_to_source_units table relates aggregated national units
                to original map units, and a Symbol_Lookup table provides definitions of all FGDC
                geologic map symbol code values (U.S. Geological Survey, 2006) used for stylizing
                the map. Where contacts seperated two different units on a source map, but not
                seperate
                polygons of the
                same national synthesis unit, those contacts have been reclassified as "internal
                contacts."</abstract>
            <purpose>This data provides a consistent depiction of the geology of the conterminous
                United States at a
                national resolution (approximately 1:500,000). It is a compilation of previously
                published maps.
                Original maps have not been modified, but additional attribution allows them to be
                displayed as a
                more consistent national depiction, while still retaining original unit
                descriptions. In some
                instances, only portions of a map have been used to isolate certain thematic
                features (e.g., Quaternary units).</purpose>
            <supplinf>ngs_gems_precambrian is a composite geodataset that conforms to GeMS (Geologic
                Map
                Schema)--a standard format for the digital publication of geologic maps", available
                at
                http://ngmdb.usgs.gov/Info/standards/GeMS/. Metadata records associated with each
                element
                within the geodataset contain more detailed descriptions of their purposes,
                constituent
                entities, and attributes.An OPEN shapefile versions of the dataset is also
                available. It
                consists of shapefiles, DBF files, and delimited text files and retains all
                information in
                the native geodatabase, but some programming will likely be necessary to assemble
                these
                components into usable formats. These metadata were prepared with the aid of script
                GeMS_FGDCMetadata.py, version of 2/27/24.</supplinf>
        </descript>
        <timeperd>
            <timeinfo>
                <rngdates>
                    <begdate>1966</begdate>
                    <enddate>2017</enddate>
                </rngdates>
            </timeinfo>
            <current>publication date</current>
        </timeperd>
        <status>
            <progress>Complete</progress>
            <update>As needed</update>
        </status>
        <spdom>
            <bounding>
                <westbc>-128.8229</westbc>
                <eastbc>-65.2549</eastbc>
                <northbc>51.6279</northbc>
                <southbc>22.5573</southbc>
            </bounding>
            <descgeog>Conterminous United States</descgeog>
        </spdom>
        <keywords>
            <theme>
                <themekt>USGS Metadata Identifier</themekt>
                <themekey>USGS:4ef33cc0-d57c-47b8-a26e-e6a6448759a5</themekey>
            </theme>
        </keywords>
        <accconst>None</accconst>
        <useconst>Unless otherwise stated, all data, metadata and related materials are considered
            to
            satisfy the quality standards relative to the purpose for which the data were collected.
            Although these data and associated metadata have been reviewed for accuracy and
            completeness
            and approved for release by the U.S. Geological Survey (USGS), no warranty expressed or
            implied is made regarding the display or utility of the data on any other system or for
            general or scientific purposes, nor shall the act of distribution constitute any such
            warranty.</useconst>
        <ptcontac>
            <cntinfo>
                <cntorgp>
                    <cntorg>U.S. Geological Survey</cntorg>
                    <cntper>NGMDB</cntper>
                </cntorgp>
                <cntaddr>
                    <addrtype>mailing</addrtype>
                    <address>12201 Sunrise Valley Dr., MS 908</address>
                    <city>Reston</city>
                    <state>VA</state>
                    <postal>20192</postal>
                </cntaddr>
                <cntvoice>NA</cntvoice>
                <cntemail>ngmdb@usgs.gov</cntemail>
            </cntinfo>
        </ptcontac>
    </idinfo>
    <dataqual>
        <attracc>
            <attraccr>Confidence that a feature exists and confidence that a feature is correctly
                identified are described in per-feature attributes ExistenceConfidence and
                IdentityConfidence.</attraccr>
        </attracc>
        <logic>Data were produced in a relational database with numerous embedded referential
            integrity
            and value range checks. Exported data was evaluated for GeMS compliance.</logic>
        <complete>Individual entries are considered complete within this data set.</complete>
        <posacc>
            <horizpa>
                <horizpar>Estimated accuracy of horizontal location is given on a per-feature basis
                    by
                    attribute LocationConfidenceMeters. Values are expected to be correct within a
                    factor of
                    2. A LocationConfidenceMeters value of -9 or -9999 indicates that no value has
                    been
                    assigned.</horizpar>
            </horizpa>
        </posacc>
        <lineage>
            <procstep>
                <procdesc>This synthesis of geology was produced by bringing together component
                    geologic maps produced in the Geologic Map Schema (GeMS) into a map synthesis
                    engine as described by: Johnstone, S.A., Colgan, J.P., and Roe, W.P., 2025, A
                    synthesis engine for constructing geologic maps of the United States: U.S.
                    Geological Survey Data Series 2025-1210, https://doi.org/10.3133/dr1210</procdesc>
                <procdate>2025</procdate>
            </procstep>
        </lineage>
    </dataqual>
    <spdoinfo>
        <direct>Vector</direct>
    </spdoinfo>
    <spref>
        <horizsys>
            <planar>
                <mapproj>
                    <mapprojn>Albers Conical Equal Area</mapprojn>
                    <albers>
                        <stdparll>29.5</stdparll>
                        <stdparll>45.5</stdparll>
                        <longcm>-96.0</longcm>
                        <latprjo>23.0</latprjo>
                        <feast>0.0</feast>
                        <fnorth>0.0</fnorth>
                    </albers>
                </mapproj>
                <planci>
                    <plance>coordinate pair</plance>
                    <coordrep>
                        <absres>0.6096</absres>
                        <ordres>0.6096</ordres>
                    </coordrep>
                    <plandu>meters</plandu>
                </planci>
            </planar>
            <geodetic>
                <horizdn>North_American_Datum_1983</horizdn>
                <ellips>GRS 1980</ellips>
                <semiaxis>6378137.0</semiaxis>
                <denflat>298.257222101</denflat>
            </geodetic>
        </horizsys>
    </spref>
    <eainfo>
        <detailed>
          <enttyp>
            <enttypl>DescriptionOfMapUnits</enttypl>
            <enttypd>Non-spatial table that captures content of the Description of Map Units (or equivalent List of Map Units and associated pamphlet text) included in a traditional paper geologic map. Has an internal hierarchy expressed by attribute HierarchyKey</enttypd>
            <enttypds>GeMS</enttypds>
          </enttyp>
          <attr>
            <attrlabl>OBJECTID</attrlabl>
            <attrdef>Internal feature number</attrdef>
            <attrdefs>ESRI</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>MapUnit</attrlabl>
            <attrdef>Short plain-text identifier of the map unit. Foreign key to DescriptionOfMapUnits table.</attrdef>
            <attrdefs>GeMS</attrdefs>
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            </attrdomv>
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            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Name</attrlabl>
            <attrdef>Name of map unit, as shown in boldface in traditional DMU, e.g., "Shnabkaib Member". Identifies unit within its hierarchical context.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>FullName</attrlabl>
            <attrdef>Name of map unit including identification of containing higher rank unit(s), e.g., "Shnabkaib Member of Moenkopi Formation".</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Age</attrlabl>
            <attrdef>Age of map unit as shown in Description of Map Units. Examples of values are "late Holocene", "Pliocene and Miocene", "Lower Cretaceous".</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Description</attrlabl>
            <attrdef>Free-format text description of map unit. Commonly structured according to one or more accepted traditions (e.g., lithology, thickness, color, weathering and outcrop characteristics, distinguishing features, genesis, age constraints) and terse.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>HierarchyKey</attrlabl>
            <attrdef>String that records hierarchical structure. Has form nn-nn-nn, nnn-nnn, or similar. Numeric, left-padded with zeros, dash-delimited. Each HierarchyKey fragment of each row MUST be the same length to allow text-based sorting of table entries.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>ParagraphStyle</attrlabl>
            <attrdef>Token that identifies formatting of paragraph(s) within traditional Description of Map Units that correspond to this table entry.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>DMUUnit3</edomv>
                <edomvd>Paragraph style for description of a second-order map unit within Description of Map Units table. Times New Roman, Regular, 10 pt, 12 pt leading, left justified, 66 pt left indent, 0 pt 1st line indent, 9 pt space before</edomvd>
                <edomvds>USGS Science Publishing Network</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>DMUUnit2</edomv>
                <edomvd>Paragraph style for description of a second-order map unit within Description of Map Units table. Times New Roman, Regular, 10 pt, 12 pt leading, left justified, 66 pt left indent, -10 pt 1st line indent, 3 pt space before</edomvd>
                <edomvds>USGS Science Publishing Network</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>DMUHeading2</edomv>
                <edomvd>Heading style for second-order headings within Description of Map Units table. Such headings are subsidiary to the primary heading "Description of Map Units". Times New Roman, bold, 10 pt, 12 pt leading, all caps, centered, 12 pt space before.</edomvd>
                <edomvds>USGS Science Publishing Network</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>DMUUnit1</edomv>
                <edomvd>Paragraph style for description of a first-order map unit within Description of Map Units table. Times New Roman, Regular, 10 pt, 12 pt leading, left justified, 66 pt left indent, -20 pt 1st line indent, 3 pt space before.</edomvd>
                <edomvds>USGS Science Publishing Network</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Label</attrlabl>
            <attrdef>Plain-text equivalent of the desired annotation for a feature: for example "14 Ma", or "^c" which (when used with the FGDC GeoAge font) results in the geologic map-unit label TRc (with TR run together to make the Triassic symbol).</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Symbol</attrlabl>
            <attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>AreaFillRGB</attrlabl>
            <attrdef>{Red, Green, Blue} tuples that specify the suggested color (e.g., "255,255,255", "124,005,255") of area fill for symbolizing MapUnit. Each color value is an integer between 0 and 255, values are zero-padded to a length of 3 digits, and values are separated by commas with no space: NNN,NNN,NNN.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>AreaFillPatternDescription</attrlabl>
            <attrdef>Text description (e.g., "random small red dashes") provided as a convenience for users who must recreate symbolization.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>DescriptionSourceID</attrlabl>
            <attrdef>Source of map-unit description; foreign key to table Datasources.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>vocab1</edomv>
                <edomvd>This Report</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>GeoMaterial</attrlabl>
            <attrdef>Categorization of map unit based on lithologic and genetic character, term selected from NGMDB standard term list defined in Appendix A of GeMS documentation, available at http://ngmdb.usgs.gov/Info/standards/GeMS..</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>Water or ice</edomv>
                <edomvd>Water or ice</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Other materials</edomv>
                <edomvd>Other materials</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Metaigneous rock</edomv>
                <edomvd>Rock derived from preexisting igneous rocks and altered by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, shear stress, and (or) chemical environment, generally at depth in Earths crust. </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coarse-grained intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Metasedimentary rock</edomv>
                <edomvd>Rock derived from preexisting sedimentary rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Quartzite</edomv>
                <edomvd>Rock derived from preexisting quartz-rich sedimentary rocks (commonly sandstone) and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, shear stress, and (or) chemical environment, generally at depth in Earths crust. </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Slate and phyllite, of sedimentary-rock origin</edomv>
                <edomvd>Fine-grained rock derived from preexisting sedimentary rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Includes phyllite and slate (compact, fine-grained rock that possesses strong cleavage and, hence, can be split into slabs and thin plates). Mostly formed from fine-grained material such as mudstone.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Rock</edomv>
                <edomvd>Various rock types, not differentiated.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Meta-carbonate rock</edomv>
                <edomvd>Rock derived from preexisting carbonate sedimentary rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Characterized by recrystallization of carbonate minerals in source rock. Includes marble (for which preexisting rock was dominantly limestone or other rock composed of calcite), dolomitic marble, meta-dolostone, and meta-dolomite (for which preexisting rock contained appreciable amount of magnesium).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Metamorphic rock</edomv>
                <edomvd>Rock derived from preexisting rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Sedimentary material</edomv>
                <edomvd>An aggregation of particles deposited by gravity, air, water, or ice, or as accumulated by other natural agents operating at Earths surface such as chemical precipitation or secretion by organisms. May include unconsolidated material (sediment) and (or) sedimentary rock. Does not include sedimentary material directly deposited as a result of volcanic activity.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Meta-ultramafic rock</edomv>
                <edomvd>Rock derived from preexisting ultramafic rocks by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Composed mostly of magnesium-bearing minerals (for example, serpentine, talc, magnesite).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coarse-grained, mafic-composition intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye. Composed mostly of feldspar and dark-colored minerals. Includes gabbroic rock.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Clastic sedimentary rock</edomv>
                <edomvd>Sedimentary rock, composed predominantly of particles or clasts derived by erosion, weathering, or mass-wasting of preexisting rock and deposited by gravity, air, water, or ice.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Medium and high-grade regional metamorphic rock, of unspecified origin</edomv>
                <edomvd>Rock derived from preexisting rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to relatively intense regional changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Origin of preexisting rock is mixed (for example, igneous and sedimentary) or is not known. Includes amphibolite, granulite, schist, and gneiss.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Sediment</edomv>
                <edomvd>Unconsolidated material (sediment) composed of particles deposited by gravity, air, water, or ice, or as accumulated by other natural agents operating at Earths surface such as chemical precipitation or secretion by organisms. Does not include sedimentary material directly deposited as a result of volcanic activity.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coarse-grained, felsic-composition intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye. Composed mostly of light-colored minerals (for example, feldspar, quartz). Includes granitic, syenitic, and monzonitic rock.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Deformation-related metamorphic rock</edomv>
                <edomvd>Rock derived from preexisting rocks by essentially solid-state mineralogical, chemical, or structural changes in response to strong deformation, commonly in association with marked changes in temperature, pressure, and (or) chemical environment. Generally forms in narrow, planar zones of local deformation (for example, along faults); characterized by foliation or alignment of mineral grains. Includes mylonite and cataclasite.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Iron-rich sedimentary rock</edomv>
                <edomvd>Sedimentary rock, in which at least half (by volume) of observed minerals are iron bearing (hematite, magnetite, limonite group minerals, siderite, iron sulfides).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>"Made" or human-engineered land</edomv>
                <edomvd>Modern, unconsolidated material known to have human-related origin.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Igneous rock</edomv>
                <edomvd>Rock and fragmental material that solidified from molten or partly molten material (magma). </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Unmapped area</edomv>
                <edomvd>Unmapped area</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Mostly sandstone</edomv>
                <edomvd>Mostly sandstone, interbedded with other sedimentary rocks that locally may include conglomerate and finer grained clastic rocks (mudstone), carbonates, and (or) coal.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Extrusive igneous material</edomv>
                <edomvd>Molten material that was erupted onto Earths surface, fusing into rock or remaining as unconsolidated particles. Includes pyroclastic flows, air-fall tephra, lava flows, and volcanic mass flows.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>GeoMaterialConfidence</attrlabl>
            <attrdef>Describes appropriateness of GeoMaterial term for describing the map unit.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>Low</edomv>
                <edomvd>The overall lithology of this map unit is not adequately classifiable using this list of terms and definitions, but the term selected is the best available.  Or this map unit is insufficiently known to confidently assign a GeoMaterial term.</edomvd>
                <edomvds>GeMS documentation</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>High</edomv>
                <edomvd>The term and definition adequately characterize the overall lithologic nature of rocks and sediments in the map unit. Regarding the subjective term "adequately characterize", we refer to context and objectives of this classification as described in the GeMS documentation.</edomvd>
                <edomvds>GeMS documentation</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Medium</edomv>
                <edomvd>The term and definition generally characterize the overall lithology of the map unit, but there are one or more significant minor lithologies that are not adequately described by the selected term.</edomvd>
                <edomvds>GeMS documentation</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>DescriptionOfMapUnits_ID</attrlabl>
            <attrdef>Primary key.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Arbitrary string. Values should be unique within this database.</udom>
            </attrdomv>
          </attr>
        </detailed>
        <detailed>
          <enttyp>
            <enttypl>DataSources</enttypl>
            <enttypd>Non-spatial table of sources of all spatial features, sources of some attributes of spatial features, and sources of some attributes of non-spatial table entries.</enttypd>
            <enttypds>GeMS</enttypds>
          </enttyp>
          <attr>
            <attrlabl>OBJECTID</attrlabl>
            <attrdef>Internal feature number</attrdef>
            <attrdefs>ESRI</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Source</attrlabl>
            <attrdef>Plain-text short description that identifies the data source.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Notes</attrlabl>
            <attrdef>Additional information specific to a particular feature or table entry.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain. Free text. Values of &lt;null&gt; or #null indicate no entry.</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>URL</attrlabl>
            <attrdef>Universal Resource Locator (URL) or Document Object Identifier (DOI), identifies a document on the World Wide Web.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>DataSources_ID</attrlabl>
            <attrdef>Primary key.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Arbitrary string. Values should be unique within this database.</udom>
            </attrdomv>
          </attr>
        </detailed>
        <detailed>
          <enttyp>
            <enttypl>Glossary</enttypl>
            <enttypd>Non-spatial table that, for certain fields (including all Type fields, Confidence fields, and GeneralLithology), lists the terms that populate these fields, term definitions, and sources for definitions.</enttypd>
            <enttypds>GeMS</enttypds>
          </enttyp>
          <attr>
            <attrlabl>OBJECTID</attrlabl>
            <attrdef>Internal feature number</attrdef>
            <attrdefs>ESRI</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Term</attrlabl>
            <attrdef>Plain-language word for a concept. Values must be unique within database as a whole.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Definition</attrlabl>
            <attrdef>Plain-language definition.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>DefinitionSourceID</attrlabl>
            <attrdef>Source of definition; foreign key to DataSources.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>vocab2</edomv>
                <edomvd>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>vocab10</edomv>
                <edomvd>USGS Science Publishing Network</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>vocab4</edomv>
                <edomvd>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>vocab3</edomv>
                <edomvd>U.S. Geological Survey, 2020, GeMS (Geologic Map Schema)--A Standard Format for the Digital Publication of Geologic Maps: U.S. Geological Survey Techniques and Methods 11-B10.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>vocab1</edomv>
                <edomvd>This Report</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Glossary_ID</attrlabl>
            <attrdef>Primary key.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Arbitrary string. Values should be unique within this database.</udom>
            </attrdomv>
          </attr>
        </detailed>
        <detailed>
          <enttyp>
            <enttypl>Source_DescriptionOfMapUnits</enttypl>
            <enttypd>Description of map units for "source" map units, those used in primary map publications used in the compilation. Source_MapUnit values are prefixed with a MapSourceID value to differentiate identically-named source map units from different source maps. Otherwise conceptually equivalent to the GeMS "DescriptionOfMapUnits" table.</enttypd>
            <enttypds>This Report</enttypds>
          </enttyp>
          <attr>
            <attrlabl>OBJECTID</attrlabl>
            <attrdef>Internal feature number</attrdef>
            <attrdefs>ESRI</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Source_MapUnit</attrlabl>
            <attrdef>Short, easily understood ASCII-character identifier for the source map unit. Prefixed with a MapSourceID value (from Source_DescriptionOfMapUnits) to differentiate identically-named source map units from different source maps. Otherwise conceptually equivalent to the "MapUnit" field in the GeMS "DescriptionOfMapUnits" table.</attrdef>
            <attrdefs>This Report</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Name</attrlabl>
            <attrdef>Name of map unit, as shown in boldface in traditional DMU, e.g., "Shnabkaib Member". Identifies unit within its hierarchical context.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>FullName</attrlabl>
            <attrdef>Name of map unit including identification of containing higher rank unit(s), e.g., "Shnabkaib Member of Moenkopi Formation".</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Age</attrlabl>
            <attrdef>Age of map unit as shown in Description of Map Units. Examples of values are "late Holocene", "Pliocene and Miocene", "Lower Cretaceous".</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Description</attrlabl>
            <attrdef>Free-format text description of map unit. Commonly structured according to one or more accepted traditions (e.g., lithology, thickness, color, weathering and outcrop characteristics, distinguishing features, genesis, age constraints) and terse.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>HierarchyKey</attrlabl>
            <attrdef>String that records hierarchical structure. Has form nn-nn-nn, nnn-nnn, or similar. Numeric, left-padded with zeros, dash-delimited. Each HierarchyKey fragment of each row MUST be the same length to allow text-based sorting of table entries.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>ParagraphStyle</attrlabl>
            <attrdef>Token that identifies formatting of paragraph(s) within traditional Description of Map Units that correspond to this table entry.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>DMUHeading2</edomv>
                <edomvd>Heading style for second-order headings within Description of Map Units table. Such headings are subsidiary to the primary heading "Description of Map Units". Times New Roman, bold, 10 pt, 12 pt leading, all caps, centered, 12 pt space before.</edomvd>
                <edomvds>USGS Science Publishing Network</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>DMUHeading5</edomv>
                <edomvd>Heading style for fifth-order headings within Description of Map Units table. Times New Roman, Italic, 10 pt, 12 pt leading, centered, 6 pt space before</edomvd>
                <edomvds>USGS Science Publishing Network</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>DMUHeading3</edomv>
                <edomvd>Heading style for third-order headings within Description of Map Units table. Times New Roman, Regular, 10 pt, 12 pt leading, all caps, centered, 10 pt space before</edomvd>
                <edomvds>USGS Science Publishing Network</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>DMUUnit2</edomv>
                <edomvd>Paragraph style for description of a second-order map unit within Description of Map Units table. Times New Roman, Regular, 10 pt, 12 pt leading, left justified, 66 pt left indent, -10 pt 1st line indent, 3 pt space before</edomvd>
                <edomvds>USGS Science Publishing Network</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>DMUUnit3</edomv>
                <edomvd>Paragraph style for description of a second-order map unit within Description of Map Units table. Times New Roman, Regular, 10 pt, 12 pt leading, left justified, 66 pt left indent, 0 pt 1st line indent, 9 pt space before</edomvd>
                <edomvds>USGS Science Publishing Network</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>DMUUnit1</edomv>
                <edomvd>Paragraph style for description of a first-order map unit within Description of Map Units table. Times New Roman, Regular, 10 pt, 12 pt leading, left justified, 66 pt left indent, -20 pt 1st line indent, 3 pt space before.</edomvd>
                <edomvds>USGS Science Publishing Network</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>DMUHeading4</edomv>
                <edomvd>Heading style for fourth-order headings within Description of Map Units table. Times New Roman, Regular, 10 pt, 12 pt leading, centered, 8 pt space before</edomvd>
                <edomvds>USGS Science Publishing Network</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Label</attrlabl>
            <attrdef>Plain-text equivalent of the desired annotation for a feature: for example "14 Ma", or "^c" which (when used with the FGDC GeoAge font) results in the geologic map-unit label TRc (with TR run together to make the Triassic symbol).</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Symbol</attrlabl>
            <attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>AreaFillRGB</attrlabl>
            <attrdef>{Red, Green, Blue} tuples that specify the suggested color (e.g., "255,255,255", "124,005,255") of area fill for symbolizing MapUnit. Each color value is an integer between 0 and 255, values are zero-padded to a length of 3 digits, and values are separated by commas with no space: NNN,NNN,NNN.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>AreaFillPatternDescription</attrlabl>
            <attrdef>Text description (e.g., "random small red dashes") provided as a convenience for users who must recreate symbolization.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>DescriptionSourceID</attrlabl>
            <attrdef>Source of map-unit description; foreign key to table Datasources.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>962</edomv>
                <edomvd>Reed, R.C., and Daniels, J., compilers., 1987, Bedrock geology of northern Michigan: Michigan Department of Natural Resources, Geological Survey Division, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>655</edomv>
                <edomvd>Tomhave, D.W., and Schulz, L.D., 2004, Bedrock geologic map showing configuration of the bedrock surface in South Dakota east of the Missouri River: South Dakota Geological Survey General Map 9, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>783</edomv>
                <edomvd>Sims, P.K., Bankey, V., Finn, C.A., 2001, Preliminary Precambrian basement map of Colorado-a geologic interpretation of the aeromagnetic anomaly map: U.S. Geological Survey Open-File Report 01-364, scale 1:1,000,000</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>632</edomv>
                <edomvd>Berg, T.M., Edmunds, W.E., Geyer, A.R., Glover, A.D., Hoskins, D.M., MacLachlan, D.B., Root, S.I., Sevon, W.D., and Socolow, A.A. 1980, Geologic map of Pennsylvania: Pennsylvania Geological Survey Map 1, Scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
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                <edomvd>Hermes, O.D., Gromet, L.P., Murray, D.P., Hamidzada, N.A., Skehan, J.W., and Mosher, S., 1994, Bedrock geologic map of Rhode Island: Rhode Island Geological Survey Rhode Island Map Series Map 1, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>674</edomv>
                <edomvd>Mudrey Jr., M.G., Brown, B.A., Greenberg, J.K., 1982, Bedrock Geologic Map of Wisconsin: Wisconsin Geological and Natural History Survey Map M-078, scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>946</edomv>
                <edomvd>Osberg, P.H., Hussey, A.M. and Boone, G.M., 1985, Bedrock geologic map of Maine: Maine Geological Survey, Geologic Map Series BGMM, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>576</edomv>
                <edomvd>Ellis, Trevor, 2016, Bedrock geologic map of the Bunceton 7.5' quadrangle, Cooper County, Missouri; Missouri Geological Survey, Open File Map, OFM-2016-672-GS, scale 1:24000. | Starbuck, E.A., 2009, Bedrock geologic map of the Luystown 7.5' quadrangle Osage County, Missouri; Missouri Geological Survey, Open-File Map, OFM-09-549-GS, scale 1:24000. | Starbuck, E.A., 2004, Bedrock geologic map of the New Melle 7.5' quadrangle St. Charles and Warren counties, Missouri; Missouri Geological Survey, Open-File Map, OFM-04-477-GS, scale 1:24000.</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1035</edomv>
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                <edomvds>This report</edomvds>
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                <edomv>955</edomv>
                <edomvd>Zen, E-an, Goldsmith, R., Ratcliffe, N.M., Robinson, P., Stanley, R.S., Hatch, N.L., Shride, A.F., Weed, E.G.A., and Wones, D.R., 1983, Bedrock geologic map of Massachusetts: U.S. Geological Survey, 3 sheets, scale 1:250,000</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>787</edomv>
                <edomvd>This Report</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>879</edomv>
                <edomvd>Spoljaric, N. and Jordan, R.R., 1966, Generalized geologic map of Delaware: Delaware Geological Survey, Special Publication 4, scale 1:297,500.</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>602</edomv>
                <edomvd>Dalton, Richard F., Monteverde, Donald H., Sugarman, Peter J., and Volkert, Richard A., compilers. Bedrock Geologic Map of New Jersey 2014. New Jersey Geological and Water Survey. 2014, Scale 1:250,000, 5 cross-sections.</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>1666</edomv>
                <edomvd>Jennings, C.W., Gutierrez, C., Bryant, W., Saucedo, G., and Wills, C., 2010, Geologic Map of California: California Geological Survey Geologic Data Map GDM-2.2010</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>871</edomv>
                <edomvd>Love, J.D., and Christiansen, A.C., 1985, Geologic map of Wyoming: U.S. Geological Survey, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>838</edomv>
                <edomvd>New Mexico Bureau of Geology and Mineral Resources, 2003, Geologic map of New Mexico: New Mexico Bureau of Geology and Mineral Resources Geologic Map, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>921</edomv>
                <edomvd>Caldwell, D.H., Erwin, R.B., and Woodward, H.P., 1968, Geologic Map of West Virginia: West Virginia Geological and Economic Survey Map 1, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>935</edomv>
                <edomvd>Gray, H.H., Ault, C.H., and Keller, S.J., 1987, Bedrock geologic map of Indiana: Indiana Geological Survey Miscellaneous Map 48, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>1065</edomv>
                <edomvd>Kansas Geological Survey, 2008, Surficial Geology of Kansas: Kansas Geological Survey, Map M-118, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>985</edomv>
                <edomvd>Sims, P.K., Peterman, Z.E., Hildebrand, T.G., and Mahan, S., 1991, Precambrian basement map of the trans-Hudson orogen and adjacent terranes, northern Great Plains, USA: U.S. Geological Survey Miscellaneous Investigations Map I-2214, scale 1:1,000,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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              <edom>
                <edomv>856</edomv>
                <edomvd>Heran, W.D., Green, G.N., and Stoeser, D.B., A digital geologic map database for Oklahoma: U.S. Geological Survey Open-File Report 03-247, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>1010</edomv>
                <edomvd>Sims, P.K., Finn, C.A., and Rystrom, V.L., 2001, USGS Open-File Report 01-199: Preliminary Precambrian Basement Map Showing Geologic-Geophysical Domains, Wyoming: U.S. Geological Survey, scale 1:1,000,000</edomvd>
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              <edom>
                <edomv>1009</edomv>
                <edomvd>This Report</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>794</edomv>
                <edomvd>Anderson, R., 2006, Geology of the Precambrian surface of Iowa and surrounding area: Iowa Geological Survey Open File Map OFM-06-7, scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>1419</edomv>
                <edomvd>Digital database of the Montana state geologic map, submitted to STATEMAP in GeMS</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>621</edomv>
                <edomvd>Bluemle, J.P., 1983, Geologic and topographic bedrock map of North Dakota: North Dakota Geological Survey Miscellaneous Map 25, scale 1:670,000</edomvd>
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              <edom>
                <edomv>591</edomv>
                <edomvd>Burchett, R.R., 1986, Geologic bedrock map of Nebraska: Nebraska Conservation and Survey Division Geologic Maps and Charts 1, scale 1:1000,000</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>579</edomv>
                <edomvd>Selves, Tyler, 2021, Bedrock geologic map of the Dover 7.5' quadrangle, Lafayette County, Missouri; Missouri Geological Survey, Open File Map, OFM-2021-712-GS, scale 1:24000.</edomvd>
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              <edom>
                <edomv>580</edomv>
                <edomvd>Wagner, Richard E. and Kisvarsanyi, Eva B., 1969, Lapilli tuffs and associated pyroclastic sediments in Upper Cambrian strata along Dent Branch, Washington County, Missouri; Missouri Geological Survey, Report of Investigations 43, RI-043, vi+80 p., 2 pls., 27 figs.</edomvd>
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              <edom>
                <edomv>1073</edomv>
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                <edomvds>This report</edomvds>
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                <edomv>623</edomv>
                <edomvd>Slucher, E.R., Swinford, E.M., Larsen, G.E., Schumacher, G.A., Shrake, D.L., Rice, C.L., Caudill, M.R., Rea, R.G., and Powers, D.M., 2006, Bedrock geologic map of Ohio: Ohio Division of Geological Survey, Map BG-1, scale 1:500,000.</edomvd>
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                <edomv>652</edomv>
                <edomvd>Horton, J.W., Jr., and Dicken, C.L., 2000, Preliminary geologic map of the Appalachian Piedmont and Blue Ridge, South Carolina segment: U.S. Geological Survey Open-File Report 01-298, scale 1:500,000</edomvd>
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                <edomv>574</edomv>
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                <edomv>799</edomv>
                <edomvd>Sims, P.K., Lund, K., Anderson, E., 2005, Precambrian Crystalline Basement Map of Idaho - An Interpreatation of Aeromagnetic Anomalies: U.S. Geological Survey Scientific Investigation Map 2884, Scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>614</edomv>
                <edomvd>Rickard, L.V., Isachsen, Y.W., and Fisher, D.W., 1970, Geologic Map of New York: New York State Museum and Science Service Map and Chart Series 15 (Explanatory sheet published in 1971), 5 sheets, scale 1:250,000</edomvd>
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              <edom>
                <edomv>666</edomv>
                <edomvd>Ratcliffe, N.M., Stanley, R.S., Gale, M.H., Thompson, P.J., Walsh, G.J., Hatch, N.L., Rankin, D.W., Doolan, B.L., Kim, Jonathan, Mehrtens, C.J., Aleinikoff, J.N., McHone, J.G., and Masonic, L.M., 2011, Bedrock Geologic Map of Vermont: U.S. Geological Survey Scientific Investigations Map SIM-3184, scale 1:100,000.</edomvd>
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                <edomv>1020</edomv>
                <edomvd>Richard, S.M., Reynolds, S.J., Spencer, J.E., and Pearthree, P.A., 2000, Geologic Map of Arizona: Arizona Geological Survey, Map 35, scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>1066</edomv>
                <edomvd>Zeller, D.E., ed., 1968, The Stratigraphic Succession in Kansas, with contributions by J.M. Jewett, C.K. Bayne, E.D. Goebel, H.G. O'Connor, A. Swineford, and D.E. Zeller: Kansas Geological Survey Bulletin 189</edomvd>
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                <edomv>887</edomv>
                <edomvd>Kolata, D.R., comp., 2005, Bedrock Geology of Illinois: Champaign, Ill., Illinois State Geological Survey, Illinois Map Series 14, scale 1:500,000.</edomvd>
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                <edomv>1084</edomv>
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                <edomv>1091</edomv>
                <edomvd>Thompson, D.E., 2011, Geologic Map of Mississippi; after Bickler, A.R., 1969, Geologic Map of Mississippi: Mississippi Department of Environmental Quality, Office of Geology, scale 1:500,000.</edomvd>
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                <edomv>1408</edomv>
                <edomvd>Walker, G.W., and MacLeod, N.S., 1991, Geologic map of Oregon: U.S. Geological Survey, scale 1:500,000</edomvd>
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                <edomv>994</edomv>
                <edomvd>McCormick, K.A., 2010, Precambrian Basement Terrane of South Dakota: South Dakota Geological Survey Bulletin 41, 2 Plates, Scale 1:1,000,000.</edomvd>
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                <edomv>1632</edomv>
                <edomvd>Schuster, J.E., 2005, Geologic map of Washington State: Washington Division of Geology and Earth Resources, Geologic Map GM-53, scale 1:500,000.</edomvd>
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                <edomv>1055</edomv>
                <edomvd>Lawton, D.E., Moye, F.J., Murray, J.B., O'Connor, B.J., Penley, H.M., Sandrock, G.S., Marsalis, W.E., Friddell, M.S., Hetrick, J.H., Huddlestun, P.F., Hunter, R.E., Mann, W.R., Martin, B.F., Pickering, S.M., Schneeberger, F.J., and Wilson, J.D., 1976, Geologic map of Georgia: Georgia Geological Survey, scale 1:500,000</edomvd>
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                <edomv>970</edomv>
                <edomvd>Milstein, R.L. compiler, 1987, Bedrock geology of southern Michigan: Michigan Department of Natural Resources Geological Publication BG-01, scale 1:500,000.</edomvd>
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                <edomv>816</edomv>
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                <edomv>874</edomv>
                <edomvd>Rodgers, John, 1985, Bedrock geological map of Connecticut: Connecticut Geological and Natural History Survey, Department of Environmental Protection, 2 sheets, scale 1:125,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
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                <edomv>1102</edomv>
                <edomvd>Hardeman, W.D., Miller, R.A., and Swingle, G.D., 1966, Geologic Map of Tennessee: Tennessee Division of Geology State Geologic Map, scale 1:250,000</edomvd>
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                <edomv>1655</edomv>
                <edomvd>Cleaves, E.T., Edwards, J., Glaser, J.D., 1968, Geologic Map of Maryland: Maryland Geological Survey, Scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>577</edomv>
                <edomvd>Thompson, Thomas L., 1995, The stratigraphic succession in Missouri (revised); Missouri Geological Survey, Volume 40-revised, 2nd series, 189 p., 42 figs., 1 tbl. | Thompson, T.L., 1970, Lower Pennsylvanian conodonts from McDonald County, Missouri; Journal of Paleontology, v. 44, p. 1041-1048, pl. 139.</edomvd>
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                <edomv>1031</edomv>
                <edomvd>McFarland, J.D., 1998 (revised 2004), Stratigraphic summary of Arkansas: Arkansas Geological Survey Circular 36, 38 p.</edomvd>
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                <edomv>1095</edomv>
                <edomvd>Martin, J.E., Sawyer, J.F., Fahrenbach, M.D., Tomhave, D.W., and Schulz, L.D., 2004, Geologic map of South Dakota: South Dakota Geological Survey General Map G-10, scale 1:500,000.</edomvd>
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                <edomv>598</edomv>
                <edomvd>Lyons, J.B., Bothner, W.A., Moench, R.H., and Thompson, J.B., Jr., 1997, Bedrock geologic map of New Hampshire: U.S. Geological Survey, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>908</edomv>
                <edomvd>Virginia Division of Mineral Resources, 1993, Geologic map of Virginia, Virginia Division of Mineral Resources, series unknown, 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>827</edomv>
                <edomvd>Sims, P.K., O'Neill, J.M., Bankey, V., and Anderson, E., 2004, Precambrian basement geologic map of Montana -- an interpretation of aeromagnetic anomalies: U.S. Geological Survey, Scientific Investigations Map SIM-2829, scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>575</edomv>
                <edomvd>Middendorf, M.A., 1999, Bedrock geologic map of the Table Rock Lake, Missouri 30' X 60' quadrangle; Missouri Geological Survey, Open-File Map, OFM-99-350-GS, scale 1:100000. | Middendorf, M.A., Thomson, K.C., Eason, G.L., and Sumner, H.S., 1987, Bedrock geologic map of the Springfield 1° X 2° quadrangle, Missouri; United States Geological Survey, Miscellaneous Field Studies Map, USGS MF-1830-D, scale 1:250000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
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                <edomv>848</edomv>
                <edomvd>North Carolina Geological Survey, 1985, Geologic map of North Carolina: North Carolina Geological Survey General Geologic Map, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
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                <edomv>835</edomv>
                <edomvd>Stewart, J.H, and Carlson, J.E., 1978, Geologic Map of Nevada: U.S. Geological Survey, scale 1:500,000</edomvd>
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                <edomv>1047</edomv>
                <edomvd>Scott, T.M., 2001, Text to accompany the geologic map of Florida: Florida Geological Survey Open-File Report 80, 30 p.</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>812</edomv>
                <edomvd>Sims, P.K., 1990, Precambrian basement map of the northern Midcontinent, U.S.A.: U.S. Geological Survey, Miscellaneous Investigations Series Map I-1853-A, scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
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                <edomv>896</edomv>
                <edomvd>Hintze, L.F., 1980, Geologic map of Utah: Utah Geological and Mineral Survey, Map A-1, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>999</edomv>
                <edomvd>Sims, P.K., 1992, Geologic map of Precambrian rocks, southern Lake Superior region, Wisconsin and northern Michigan: U.S. Geological Survey Miscellaneous Investigations Series Map I-2185, scale: 1:500,000</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
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                <edomv>578</edomv>
                <edomvd>Kisvarsanyi, Eva B, 1981, Geology of the Precambrian St. Francois terrane, southeastern Missouri; Missouri Geological Survey, Report of Investigations 64 (Contribution to Precambrian Geology No. 8), vi+58 p., 1 pl., 9 figs., 10 tbls.</edomvd>
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                <edomv>1645</edomv>
                <edomvd>Osborne, W.E., Szabo, M.W., Copeland Jr., C.W., and Neathery, T.L., 1989, Geologic Map of Alabama: Geological Survey of Alabama Special Map 221, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>940</edomv>
                <edomvd>Witzke, B.J., Anderson, R.R., and Pope, J.P., 2010, Bedrock Geologic Map of Iowa: Iowa Geological Survey Open-File Map OFM-2010-01, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>1115</edomv>
                <edomvd>Texas Water Science Center, 2015, Geologic database of Texas</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1652</edomv>
                <edomvd>Lewis, R.S., Link, P.K., Stanford, L.R., and Long, S.P., 2012, Geologic map of Idaho: Idaho Geological Survey, Map M-9, scale 1:750,000.</edomvd>
                <edomvds>This report</edomvds>
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          </attr>
          <attr>
            <attrlabl>GeoMaterial</attrlabl>
            <attrdef>Categorization of map unit based on lithologic and genetic character, term selected from NGMDB standard term list defined in Appendix A of GeMS documentation, available at http://ngmdb.usgs.gov/Info/standards/GeMS..</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>Eolian sediment</edomv>
                <edomvd>Silt- and sand-sized sediment, deposited by wind.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coastal zone sediment</edomv>
                <edomvd>Mud and sand, with lesser amounts of gravel, deposited on beaches, on barrier islands, or in nearshore-marine, deltaic, or various low-energy shoreline (mud flat, tidal flat, sabka, algal flat) environments.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Metasedimentary rock</edomv>
                <edomvd>Rock derived from preexisting sedimentary rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Chert</edomv>
                <edomvd>Sedimentary rock, composed chiefly of microcrystalline or cryptocrystalline quartz.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coastal zone sediment, mostly coarse-grained</edomv>
                <edomvd>Mostly sand, silt, and gravel, deposited on beaches, in dunes, and in shallow-marine and related alluvial environments.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Igneous and metamorphic rock</edomv>
                <edomvd>Consists of coarse-grained intrusive igneous rock and generally medium- to high-grade metamorphic rock.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Meta-ultramafic rock</edomv>
                <edomvd>Rock derived from preexisting ultramafic rocks by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Composed mostly of magnesium-bearing minerals (for example, serpentine, talc, magnesite).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Debris flows, landslides, and other localized mass-movement sediment</edomv>
                <edomvd>Sediment formed by relatively localized, downslope transport of particles or clasts produced by weathering and breakdown of underlying rock, sediment, and (or) soil. Composed of poorly sorted and poorly stratified material that ranges in size from clay to boulders. Speed of downslope transport ranges from rapid to imperceptible.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Lacustrine sediment, mostly coarse-grained</edomv>
                <edomvd>Mostly well-sorted and well-bedded material, generally sand and gravel sized, with lesser amounts of silt and clay, deposited in perennial to intermittent lakes. Much of sediment is derived from material eroded and transported by streams. Mostly deposits of lake-marginal beaches and deltas.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Medium and high-grade regional metamorphic rock, of unspecified origin</edomv>
                <edomvd>Rock derived from preexisting rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to relatively intense regional changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Origin of preexisting rock is mixed (for example, igneous and sedimentary) or is not known. Includes amphibolite, granulite, schist, and gneiss.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Alluvial sediment</edomv>
                <edomvd>Unconsolidated material deposited by streams or other bodies of running water as sorted or semisorted sediment in streambed, or on its floodplain or delta, or as cone or fan at base of mountain slope. Grain size varies from clay to gravel.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Meta-volcaniclastic rock</edomv>
                <edomvd>Rock derived from preexisting volcaniclastic rocks by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Composed of deformed but recognizable particles or clasts of volcanic explosive material.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Intermediate-composition lava flows</edomv>
                <edomvd>Lateral, surficial outpourings of molten lava from vent or fissure; also, solidified bodies of rock that form when they cool. Parental magma commonly erupts from stratovolcanoes as thick lava flows. Includes rocks that are, in color and in mineral composition, intermediate between felsic and mafic rocks (for example, andesite).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Pyroclastic flows</edomv>
                <edomvd>Hot ash, pumice, and rock fragments erupted from volcano or caldera. Material moves downslope commonly in chaotic flows; once deposited, hot fragments may compact under their own weight and weld together.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Carbonate rock</edomv>
                <edomvd>Sedimentary rock, consisting chiefly of carbonate minerals such as limestone or dolomite. </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>"Made" or human-engineered land</edomv>
                <edomvd>Modern, unconsolidated material known to have human-related origin.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Playa sediment</edomv>
                <edomvd>Fine-grained clastic sediment and evaporitic salts, deposited in ephemeral lakes in centers of undrained basins. Includes material deposited in playas, mud flats, salt flats, and adjacent saline marshes. Generally interbedded with eolian sand and with lacustrine sediment deposited during wetter climatic periods; commonly intertongues upslope with sediment deposited by alluvial fans.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Unmapped area</edomv>
                <edomvd>Unmapped area</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Alluvial sediment, mostly coarse-grained</edomv>
                <edomvd>Unconsolidated material deposited by streams or other bodies of running water as sorted or semisorted sediment in streambed, or on its floodplain or delta, or as cone or fan at base of mountain slope. Sediment is mostly sand, gravel, and coarser material but may also contain some silt and clay.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Sedimentary and extrusive igneous material</edomv>
                <edomvd>Either (1) sedimentary rock and (or) unconsolidated material (sediment) and extrusive igneous material (volcanic rock and [or] sediment) or (2) volcanic rock and (or) sediment and such material after erosion and redeposition.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Metaigneous rock</edomv>
                <edomvd>Rock derived from preexisting igneous rocks and altered by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, shear stress, and (or) chemical environment, generally at depth in Earths crust. </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coarse-grained intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Meta-felsic and intermediate rock</edomv>
                <edomvd>Rock derived from preexisting felsic and intermediate-composition rocks by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Composed mostly of light-colored minerals; relatively enriched in silica. Includes metagranite, metadiorite, and meta-andesite.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Marine sediment, mostly coarse-grained</edomv>
                <edomvd>Mud, sand, and gravel eroded from rocks and sediment on land, transported by streams, and deposited in marine deltas and basins. Mostly siliceous in composition.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Dolomite</edomv>
                <edomvd>Carbonate sedimentary rock, consisting chiefly of dolomite. Although dolostone is the proper analog to limestone, it has not often been applied to dolomitic units.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Lacustrine sediment, mostly fine-grained</edomv>
                <edomvd>Mostly well-sorted and well-bedded material, generally silt and clay sized, with lesser amounts of sand, deposited in perennial to intermittent lakes. </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coal and lignite</edomv>
                <edomvd>Organic-rich sedimentary rock, formed from compaction and alteration of plant remains. Coal is consolidated, harder, black rock. Lignite is semiconsolidated, brown to black, earthy material that may contain large particles of recognizable plant parts and tends to crack upon drying.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Slate and phyllite, of sedimentary-rock origin</edomv>
                <edomvd>Fine-grained rock derived from preexisting sedimentary rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Includes phyllite and slate (compact, fine-grained rock that possesses strong cleavage and, hence, can be split into slabs and thin plates). Mostly formed from fine-grained material such as mudstone.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coastal zone sediment, mostly fine-grained</edomv>
                <edomvd>Mostly clay and silt, deposited in lagoons, tidal flats, backbarriers, and coastal marshes.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Sand and gravel of unspecified origin</edomv>
                <edomvd>Sediment composed mostly of sand and (or) gravel, formed by weathering and erosion of preexisting rocks or minerals; eroded particles or clasts are transported and deposited by gravity, air, water, or ice.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Sedimentary material</edomv>
                <edomvd>An aggregation of particles deposited by gravity, air, water, or ice, or as accumulated by other natural agents operating at Earths surface such as chemical precipitation or secretion by organisms. May include unconsolidated material (sediment) and (or) sedimentary rock. Does not include sedimentary material directly deposited as a result of volcanic activity.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Loess</edomv>
                <edomvd>Silty sediment, deposited by wind, commonly near glacial margin.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Conglomerate</edomv>
                <edomvd>Sedimentary rock, composed predominantly of particles or clasts derived by erosion and weathering of preexisting rock; contains more than 30 percent gravel-sized clasts.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Mostly mudstone</edomv>
                <edomvd>Mostly mudstone, interbedded with other sedimentary rocks that locally may include coarser grained clastic rocks (sandstone, conglomerate), carbonates, and (or) coal.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Alluvial sediment, mostly fine-grained</edomv>
                <edomvd>Unconsolidated material deposited by streams or other bodies of running water as sorted or semisorted sediment in streambed, or on its floodplain or delta, or as cone or fan at base of mountain slope. Sediment is mostly silt and clay but may also contain some sand and gravel.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Intermediate-composition pyroclastic flows</edomv>
                <edomvd>Hot ash, pumice, and rock fragments erupted from volcano. Material moves downslope commonly in chaotic flows; once deposited, hot fragments may compact under their own weight and weld together. Parental magma commonly erupts from stratovolcanoes as thick lava flows but also can generate strong explosive eruptions to form pyroclastic flows. Includes rocks that are, in color and mineral composition, intermediate between felsic and mafic rocks (for example, andesite).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Limestone</edomv>
                <edomvd>Carbonate sedimentary rock, consisting chiefly of calcite.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coarse-grained, intermediate-composition intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye. Intermediate in color and in mineral composition (between felsic and mafic igneous rock). Includes dioritic rock.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Dune sand</edomv>
                <edomvd>Mostly sand-sized sediment, deposited by wind. Typically characterized by various dune landforms.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Exotic-composition intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) below Earths surface that has exotic mineralogical, textural, or field setting characteristics. Typically dark colored with abundant phenocrysts. Includes kimberlite, lamprophyre, lamproite, and foiditic rocks.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Marine sediment</edomv>
                <edomvd>Mud and sand, deposited in various marine environments. May originate from erosion of rocks and sediment or may be derived from marine organisms (of carbonate or siliceous composition).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Ultramafic intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye. Composed almost entirely of mafic minerals (for example, hypersthene, augite, olivine).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Sedimentary rock</edomv>
                <edomvd>Consolidated material (rock) composed of particles transported and deposited by gravity, air, water, or ice, or accumulated by other natural agents operating at Earths surface, such as chemical precipitation or secretion by organisms. Does not here include sedimentary material directly deposited as result of volcanic activity.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Contact-metamorphic rock</edomv>
                <edomvd>Altered rock that originated by local processes of thermal metamorphism, genetically related to intrusion and extrusion of magmas and taking place at or near contact with body of igneous rock. Metamorphic changes are effected by heat and fluids emanating from magma and by some deformation because of emplacement of igneous mass.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Igneous rock</edomv>
                <edomvd>Rock and fragmental material that solidified from molten or partly molten material (magma). </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Lava flows</edomv>
                <edomvd>Lateral, surficial outpourings of molten lava from vent or fissure; also, solidified bodies of rock that form when they cool. Composed generally of fine-grained, dark-colored rocks (for example, basalt), which tend to form extensive sheets that have generally low relief, except in vent areas where cinder cones or shield volcanoes may form. Includes basaltic shield volcanoes, which may become very large (for example, Hawaii).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Mafic-composition pyroclastic flows</edomv>
                <edomvd>Hot ash, pumice, and rock fragments erupted from volcano. Material moves downslope commonly in chaotic flows; once deposited, hot fragments may compact under their own weight and weld together. Because of their low silica content and resulting low viscosity, parental magmas tend to erupt gently as lava flows rather than more forcefully as pyroclastic flows. Includes basalt; rocks are commonly dark-colored. </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Silt and clay of unspecified origin</edomv>
                <edomvd>Sediment composed mostly of silt and (or) clay, formed by weathering and erosion of preexisting rocks or minerals; eroded particles or clasts are transported and deposited by gravity, air, water, or ice.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Marine sediment, mostly fine-grained</edomv>
                <edomvd>Mostly clay- and silt-sized sediment, deposited in relatively deep, quiet water, far removed from areas where coarser grained clastic sediments are washed into marine environment. Includes sediment derived from marine organisms.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Evaporitic rock</edomv>
                <edomvd>Sedimentary rock, composed primarily of minerals produced by evaporation of saline solution. Examples include gypsum, anhydrite, other diverse sulfates, halite (rock salt), primary dolomite, and rocks composed of various nitrates and borates.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Glacial till</edomv>
                <edomvd>Mostly unsorted and unstratified material, generally unconsolidated, deposited directly by and underneath or adjacent to glacier without subsequent reworking by meltwater. Consists of heterogeneous mixture of clay, silt, sand, gravel, and boulders, ranging widely in size and shape.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Quartzite</edomv>
                <edomvd>Rock derived from preexisting quartz-rich sedimentary rocks (commonly sandstone) and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, shear stress, and (or) chemical environment, generally at depth in Earths crust. </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) below Earths surface.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Metamorphic rock</edomv>
                <edomvd>Rock derived from preexisting rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Volcaniclastic (fragmental) material</edomv>
                <edomvd>Rock and unconsolidated material consisting of particles or clasts that were formed by volcanic explosion or aerial expulsion from volcanic vent.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Mafic-composition lava flows</edomv>
                <edomvd>Lateral, surficial outpourings of molten lava from vent or fissure; also, solidified bodies of rock that form when they cool. Low-silica parental magmas have low viscosity and tend to form extensive sheets that have generally low relief. Includes basaltic shield volcanoes, which may become very large (for example, in Hawaii). Composed of fine-grained, dark rocks, including basaltic.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Colluvium and other widespread mass-movement sediment</edomv>
                <edomvd>Sediment formed by slow, relatively widespread, downslope transport of particles or clasts produced by weathering and breakdown of underlying rock, sediment, and (or) soil. Composed of poorly sorted and poorly stratified material that ranges in size from clay to boulders.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Sandstone</edomv>
                <edomvd>Sedimentary rock, composed predominantly of particles or clasts derived by erosion and weathering of preexisting rock; consists mostly of sand-sized particles, with or without fine-grained matrix of silt or clay.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Fine-grained intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at shallow depth beneath Earths surface, thereby cooling quickly. Generally fine grained but may contain large mineral crystals (phenocrysts). Mostly found as tabular dikes or sills.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Sediment</edomv>
                <edomvd>Unconsolidated material (sediment) composed of particles deposited by gravity, air, water, or ice, or as accumulated by other natural agents operating at Earths surface such as chemical precipitation or secretion by organisms. Does not include sedimentary material directly deposited as a result of volcanic activity.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Deformation-related metamorphic rock</edomv>
                <edomvd>Rock derived from preexisting rocks by essentially solid-state mineralogical, chemical, or structural changes in response to strong deformation, commonly in association with marked changes in temperature, pressure, and (or) chemical environment. Generally forms in narrow, planar zones of local deformation (for example, along faults); characterized by foliation or alignment of mineral grains. Includes mylonite and cataclasite.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Iron-rich sedimentary rock</edomv>
                <edomvd>Sedimentary rock, in which at least half (by volume) of observed minerals are iron bearing (hematite, magnetite, limonite group minerals, siderite, iron sulfides).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Felsic-composition lava flows</edomv>
                <edomvd>Lateral, surficial outpourings of molten lava from vent or fissure; also, solidified bodies of rock that form when they cool. Because of their high silica content and resulting high viscosity, parental magmas tend to erupt explosively, and so these deposits are uncommon. Includes fine-grained, light-colored rock with rhyolitic, dacitic, trachytic, and latitic composition.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Sandstone and mudstone</edomv>
                <edomvd>Sandstone and mudstone (including shale and siltstone), in approximately equal (or unspecified) proportions. </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Intermediate-composition air-fall tephra</edomv>
                <edomvd>Fragments of volcanic rock and lava, of various sizes, carried into the air by explosions and by hot gases in eruption columns or lava fountains; known as tephra. As tephra falls to ground, with increasing distance from volcano, average size of individual rock particles and thickness of resulting deposit decrease. Parental magma commonly erupts from stratovolcanoes as thick lava flows but also can generate strong explosive eruptions to form pyroclastic flows. Includes rocks that are, in color and mineral composition, intermediate between felsic and mafic rocks (for example, andesite). </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Residual material</edomv>
                <edomvd>Unconsolidated material, developed in place by weathering of underlying rock or sediment. Usually forms relatively thin surface layer that conceals unweathered or partly altered source material. Material from which soils are formed.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Mostly sandstone</edomv>
                <edomvd>Mostly sandstone, interbedded with other sedimentary rocks that locally may include conglomerate and finer grained clastic rocks (mudstone), carbonates, and (or) coal.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Clastic sediment</edomv>
                <edomvd>Sediment formed by weathering and erosion of preexisting rocks or minerals; eroded particles or clasts are transported and deposited by gravity, air, water, or ice.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Water or ice</edomv>
                <edomvd>Water or ice</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Ice-contact and ice-marginal sediment</edomv>
                <edomvd>Mostly sand-, silt-, and gravel-sized particles or clasts derived from rock or preexisting sediment that has been eroded and transported by glaciers. As glacier melted, material was deposited by running water essentially in contact with glacial ice or was transported and deposited by glacially fed streams. Includes sediment deposited into water bodies adjacent to glacier.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Felsic-composition pyroclastic flows</edomv>
                <edomvd>Hot ash, pumice, and rock fragments erupted from volcano or caldera. Material moves downslope commonly in chaotic flows; once deposited, hot fragments may compact under their own weight and weld together. Because of their high-silica content and resulting high viscosity, parental magmas tend to erupt explosively. Includes rhyolite, dacite, trachyte, latite; rocks are commonly light-colored.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Fine-grained, intermediate-composition intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at shallow depth beneath Earths surface, thereby cooling quickly. Generally fine grained but may contain large mineral crystals (phenocrysts). Mostly found as tabular dikes or sills. Intermediate in color and in mineral composition (between felsic and mafic igneous rock). Includes andesitic rock.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Mostly carbonate rock</edomv>
                <edomvd>Mostly carbonate rock, interbedded with other sedimentary rock types.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Regional metamorphic rock, of unspecified origin</edomv>
                <edomvd>Rock derived from preexisting rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked regional changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Origin of preexisting rock is mixed (for example, igneous and sedimentary) or is not known. </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Mudstone</edomv>
                <edomvd>Sedimentary rock, composed predominantly of particles or clasts derived by erosion and weathering of preexisting rock; consists mostly of mud (that is, silt- and clay-sized particles). Includes shale and siltstone.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Lower-grade metamorphic rock, of unspecified origin</edomv>
                <edomvd>Rock derived from preexisting rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to relatively mild regional changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Origin of preexisting rock is mixed (for example, igneous and sedimentary) or is not known. Includes slate and phyllite.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Carbonate sediment</edomv>
                <edomvd>Sediment formed by biotic or abiotic precipitation from aqueous solution of carbonates of calcium, magnesium, or iron (for example, limestone, dolomite).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Fine-grained, felsic-composition intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at shallow depth beneath Earths surface, thereby cooling quickly. Generally fine grained but may contain large mineral crystals (phenocrysts). Mostly found as tabular dikes or sills. Composed mostly of light-colored minerals. Includes rhyolitic, dacitic, trachytic, and latitic rock.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Rock</edomv>
                <edomvd>Various rock types, not differentiated.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Meta-carbonate rock</edomv>
                <edomvd>Rock derived from preexisting carbonate sedimentary rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Characterized by recrystallization of carbonate minerals in source rock. Includes marble (for which preexisting rock was dominantly limestone or other rock composed of calcite), dolomitic marble, meta-dolostone, and meta-dolomite (for which preexisting rock contained appreciable amount of magnesium).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Peat and muck</edomv>
                <edomvd>Unconsolidated material, principally composed of plant remains, with lesser amounts of fine-grained clastic sediment. Deposited in water-saturated environment such as swamp, marsh, or bog. With lithification, such material becomes coal.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Felsic-composition air-fall tephra</edomv>
                <edomvd>Fragments of volcanic rock and lava, of various sizes, carried into air by explosions and by hot gases in eruption columns or lava fountains; known as tephra. As tephra falls to ground, with increasing distance from volcano, average size of individual rock particles and thickness of resulting deposit decrease. Because of their high silica content and resulting high viscosity, felsic-composition magmas tend to erupt explosively, readily forming pumice and volcanic ash. Composed of light-colored rocks (for example, rhyolite, dacite, trachyte, latite). </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Schist and gneiss, of sedimentary-rock origin</edomv>
                <edomvd>Foliated rock derived from preexisting sedimentary rocks by essentially solid-state mineralogical, chemical, or structural changes in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Includes schist (characterized by such strong foliation or alignment of minerals that it readily splits into flakes or slabs) and gneiss (characterized by alternating, irregular bands of different mineral composition). Mostly formed from fine-grained material such as mudstone.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coarse-grained, mafic-composition intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye. Composed mostly of feldspar and dark-colored minerals. Includes gabbroic rock.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Clastic sedimentary rock</edomv>
                <edomvd>Sedimentary rock, composed predominantly of particles or clasts derived by erosion, weathering, or mass-wasting of preexisting rock and deposited by gravity, air, water, or ice.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Volcanic mass flow</edomv>
                <edomvd>Volcanic deposits formed by mass movement (for example, debris avalanches, debris flows, lahar deposits), in many cases triggered by volcanic eruption. Debris avalanches that occur on volcanoes clearly without eruptive trigger may be classified as sedimentary (for example, as Debris flows, landslides, and other localized mass-movement sediment).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coarse-grained, felsic-composition intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye. Composed mostly of light-colored minerals (for example, feldspar, quartz). Includes granitic, syenitic, and monzonitic rock.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Meta-mafic rock</edomv>
                <edomvd>Rock derived from preexisting mafic rocks by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Composed mostly of iron- and magnesium-bearing, dark-colored and (or) green minerals. Includes greenstone, amphibolite, and metagabbro.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Lacustrine sediment</edomv>
                <edomvd>Mostly well-sorted and well-bedded material that ranges in grain size from clay to gravel, deposited in perennial to intermittent lakes. Much of sediment is derived from material eroded and transported by streams. Includes deposits of lake-marginal beaches and deltas.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Fine-grained, mafic-composition intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at shallow depth beneath Earths surface, thereby cooling quickly. Generally fine grained but may contain large mineral crystals (phenocrysts). Mostly found as tabular dikes or sills. Composed mostly of dark-colored minerals. Includes basaltic rock.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Ice-contact and ice-marginal sediment, mostly coarse-grained</edomv>
                <edomvd>Mostly sand- and gravel-sized particles or clasts, with lesser amounts of silt and clay, derived from rock or preexisting sediment that has been eroded and transported by glaciers. As glacier melted, material was deposited by running water essentially in contact with glacial ice or was transported and deposited by glacially fed streams. Includes sediment deposited into water bodies adjacent to glacier.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Extrusive igneous material</edomv>
                <edomvd>Molten material that was erupted onto Earths surface, fusing into rock or remaining as unconsolidated particles. Includes pyroclastic flows, air-fall tephra, lava flows, and volcanic mass flows.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>GeoMaterialConfidence</attrlabl>
            <attrdef>Describes appropriateness of GeoMaterial term for describing the map unit.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>Low</edomv>
                <edomvd>Either (1) the overall lithologic nature of rocks and (or) sediments in this map unit is not adequately classifiable using the available list of GeoMaterial terms (and their definitions), but the selected term is the best available, or (2) this map unit is not sufficiently known enough to confidently assign a GeoMaterial term.</edomvd>
                <edomvds>U.S. Geological Survey, 2020, GeMS (Geologic Map Schema)--A Standard Format for the Digital Publication of Geologic Maps: U.S. Geological Survey Techniques and Methods 11-B10.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>High</edomv>
                <edomvd>The selected term in the GeoMaterial field (and its definition) adequately characterizes the overall lithologic nature of rocks and (or) sediments in the map unit.</edomvd>
                <edomvds>U.S. Geological Survey, 2020, GeMS (Geologic Map Schema)--A Standard Format for the Digital Publication of Geologic Maps: U.S. Geological Survey Techniques and Methods 11-B10.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Medium</edomv>
                <edomvd>The selected term in the GeoMaterial field (and its definition) generally characterizes the overall lithologic nature of rocks and (or) sediments in the map unit, but one or more significant but minor lithologies are not adequately described by the selected term.</edomvd>
                <edomvds>U.S. Geological Survey, 2020, GeMS (Geologic Map Schema)--A Standard Format for the Digital Publication of Geologic Maps: U.S. Geological Survey Techniques and Methods 11-B10.</edomvds>
              </edom>
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            <attrdef>Primary key on the Source_DescriptionOfMapUnits table.</attrdef>
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        <detailed>
          <enttyp>
            <enttypl>Synthesis_to_Source_Units</enttypl>
            <enttypd>Table defining relationships between "source map units" and synthesis "map units".</enttypd>
            <enttypds>This Report</enttypds>
          </enttyp>
          <attr>
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            <attrdef>Internal feature number</attrdef>
            <attrdefs>ESRI</attrdefs>
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              <udom>Unrepresentable domain</udom>
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          <attr>
            <attrlabl>MapSourceID</attrlabl>
            <attrdef>Identifies source map. Foreign key to DataSources table.</attrdef>
            <attrdefs>This Report</attrdefs>
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              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Source_DescriptionOfMapUnitsID</attrlabl>
            <attrdef>Foreign key to DescriptionOfMapUnits table.</attrdef>
            <attrdefs>This Report</attrdefs>
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              <udom>Unrepresentable domain</udom>
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          <attr>
            <attrlabl>Source_MapUnit</attrlabl>
            <attrdef>Short, easily understood ASCII-character identifier for the source map unit. Prefixed with a MapSourceID value (from Source_DescriptionOfMapUnits) to differentiate identically-named source map units from different source maps. Otherwise conceptually equivalent to the "MapUnit" field in the GeMS "DescriptionOfMapUnits" table.</attrdef>
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            <attrdef>Foreign key to DescriptionOfMapUnits table.</attrdef>
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          <attr>
            <attrlabl>MapUnit</attrlabl>
            <attrdef>Short plain-text identifier of the map unit. Foreign key to DescriptionOfMapUnits table.</attrdef>
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              <edom>
                <edomv>Ygg</edomv>
                <edomvd>Granitic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>pC</edomv>
                <edomvd>Undifferentiated Precambrian rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Aum</edomv>
                <edomvd>Ultramafic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Ai</edomv>
                <edomvd>Intrusive rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>PZpCm</edomv>
                <edomvd>Metamorphic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Zu</edomv>
                <edomvd>Undifferentiated Neoproterozoic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>PZpCu</edomv>
                <edomvd>Undifferentiated Paleozoic to Precambrian rocks</edomvd>
                <edomvds>This Report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>Ymc</edomv>
                <edomvd>Carbonate and meta-carbonate rocks</edomvd>
                <edomvds>This Report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>Zm</edomv>
                <edomvd>Metamorphic and igneous rocks</edomvd>
                <edomvds>This Report</edomvds>
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              <edom>
                <edomv>Xu</edomv>
                <edomvd>Undifferentiated Paleoproterozoic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Ymss</edomv>
                <edomvd>Clastic sedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>Au</edomv>
                <edomvd>Undifferentiated Archean rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Xif</edomv>
                <edomvd>Iron formation</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Aig</edomv>
                <edomvd>Granitic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Yms</edomv>
                <edomvd>Sedimentary and metasedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>Ymg</edomv>
                <edomvd>Mafic intrusive rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>PRu</edomv>
                <edomvd>Undifferentiated Proterozoic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Xim</edomv>
                <edomvd>Gabbro and mafic lava flows</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>CAZms</edomv>
                <edomvd>Metasedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>water</edomv>
                <edomvd>Water and ice</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Xmsq</edomv>
                <edomvd>Quartzite</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Zg</edomv>
                <edomvd>Granitic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>af</edomv>
                <edomvd>Artificial fill</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Xi</edomv>
                <edomvd>Igneous and metaigneous rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>unmapped</edomv>
                <edomvd>Unmapped areas</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Yl</edomv>
                <edomvd>Igneous rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>PHs</edomv>
                <edomvd>Phanerozoic cover rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Zms</edomv>
                <edomvd>Metasedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>PZpCg</edomv>
                <edomvd>Igneous rocks</edomvd>
                <edomvds>This Report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>Ams</edomv>
                <edomvd>Metasedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>PZpCms</edomv>
                <edomvd>Metasedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Xig</edomv>
                <edomvd>Granitic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Zmg</edomv>
                <edomvd>Metaigneous rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>scz</edomv>
                <edomvd>Shear zone rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Yu</edomv>
                <edomvd>Undifferentiated Mesoproterozoic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>PRum</edomv>
                <edomvd>Ultramafic rocks</edomvd>
                <edomvds>This Report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>Xms</edomv>
                <edomvd>Metasedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>PHi</edomv>
                <edomvd>Phanerozoic igneous rocks</edomvd>
                <edomvds>This Report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>PZpCmg</edomv>
                <edomvd>Metaigneous rocks</edomvd>
                <edomvds>This Report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>Xmss</edomv>
                <edomvd>Slate and sandstone</edomvd>
                <edomvds>This Report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>PZpCum</edomv>
                <edomvd>Ultramafic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Aif</edomv>
                <edomvd>Iron formation</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Zs</edomv>
                <edomvd>Clastic sedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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          </attr>
        </detailed>
        <detailed>
          <enttyp>
            <enttypl>Symbol_Lookup</enttypl>
            <enttypd>FGDC symbols used in the source maps referenced herein.</enttypd>
            <enttypds>This Report</enttypds>
          </enttyp>
          <attr>
            <attrlabl>OBJECTID</attrlabl>
            <attrdef>Internal feature number</attrdef>
            <attrdefs>ESRI</attrdefs>
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              <udom>Unrepresentable domain</udom>
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          <attr>
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              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Symbol</attrlabl>
            <attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>IsConcealed</attrlabl>
            <attrdef>Flag for contacts and faults covered by overlying map unit.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>LocationConfidenceMeters</attrlabl>
            <attrdef>Estimated half-width in meters of positional uncertainty envelope; position is relative to other features in database.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Positive real number. Value of -9, -99, or -999 indicates value is unknown.</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Type</attrlabl>
            <attrdef>Classifier that specifies what kind of geologic feature is represented by a database element: that a certain line within feature class ContactsAndFaults is a contact, or thrust fault, or water boundary; or that a point in GeochronPoints represents a K-Ar date.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>reverse fault</edomv>
                <edomvd>A fault on which the hanging wall has moved upward relative to the footwall. The dip of the fault is usually greater than 45°.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>caldera margin</edomv>
                <edomvd>[The margin of] a large, basin-shaped volcanic depression, more or less circular or cirquelike in form, the diameter of which is many times greater than that of the included vent or vents, no matter what the steepness of the walls or form of the floor (Williams, 1941). It is formed by collapse during an eruption.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>shoreline</edomv>
                <edomvd>A line delineating the boundary of a body of water, such as a river, lake, or the ocean</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>internal contact</edomv>
                <edomvd>A planar or irregular surface separating different portions of the same geologic map unit, such as individual landslide blocks with a mapped landslide, or separately emplaced portions of a composite plutonic unit.</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>strike-slip fault, right lateral offset</edomv>
                <edomvd>A strike-slip fault on which the side opposite the observer has been displaced to the right.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>thrust fault</edomv>
                <edomvd>A fault with a dip of 45° or less over much of its extent, on which the hanging wall has moved upward relative to the footwall.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>gradational contact</edomv>
                <edomvd>A contact defined by a gradual or continuous lithologic change from one geologic map unit to another.</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>contact</edomv>
                <edomvd>A plane or irregular surface between two types or ages of rock.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>oblique-slip fault, left lateral offset</edomv>
                <edomvd>A fault on which the net slip has dip slip and strike slip components, and the side opposite the observer has been displaced to the left.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>normal fault</edomv>
                <edomvd>A fault in which the hanging wall has moved downward relative to the footwall. The angle of the fault is usually 45-90 degrees, and in most cases close to 60 degrees.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>overturned thrust fault</edomv>
                <edomvd>A fault with an original dip of 45° or less over much of its extent, on which the hanging wall has moved upward relative to the footwall, that has subsequently been rotated beyond perpendicular so that the primary hanging wall and footwall positioning have been reversed.</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>shear zone</edomv>
                <edomvd>A discrete, parallel-sided zone of localized shearing displacement, which may be recognized by sigmoidal mineral-filled veins, locally well-developed cleavage or foliation, wholesale grain-size reduction or mylonitization, or some combination of these features.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>detachment fault</edomv>
                <edomvd>A regionally extensive, gently dipping normal fault that is commonly associated with extension in a metamorphic core complex.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>glacial terminus</edomv>
                <edomvd>The lower margin or extremity of a glacier, referring to the maximum extent (limit) reached by the glacier.</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>strike-slip fault, left lateral offset</edomv>
                <edomvd>A strike-slip fault on which the side opposite the observer has been displaced to the left.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>scratch boundary</edomv>
                <edomvd>Arbitrary, non-physical boundary between map units on a geologic map. For example, between an undivided unit and its subunits, or between different names for the same package of rocks.</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>lineament</edomv>
                <edomvd>A linear feature that has been determined from aerial photographs or remotely sensed data but not identified on the ground.</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>key bed</edomv>
                <edomvd>A well-defined, easily identifiable stratum or body of strata that has sufficiently distinctive characteristics (such as lithology or fossil content) to facilitate correlation in field mapping or subsurface work.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>fault</edomv>
                <edomvd>A discrete surface or zone of discrete surfaces separating two rock masses across which one mass has slid past the other.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>listric fault</edomv>
                <edomvd>A curved downward-flattening fault, generally concave upward. Listric faults may be characterized by normal or reverse separation, but the term is used most frequently in normal faulting and is often a characteristic of growth faults.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>low-angle normal fault</edomv>
                <edomvd>A fault in which the hanging wall has moved downward relative to the footwall. The angle of the fault is less than 45 degrees.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>oblique-slip fault, right lateral offset</edomv>
                <edomvd>A fault on which the net slip has dip slip and strike slip components, and the side opposite the observer has been displaced to the right.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>map boundary</edomv>
                <edomvd>The boundary of the map. In a GIS database, the line that bounds the outer extent of the polygons.</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>SymbolClass</attrlabl>
            <attrdef>Short description of which class of vector features this symbol applies to; line, point, or fill.</attrdef>
            <attrdefs>This Report</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>ExistenceConfidence</attrlabl>
            <attrdef>Confidence that feature exists.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>questionable</edomv>
                <edomvd>Identity of a feature cannot be determined using relevant observations and scientific judgment; therefore, one cannot be reasonably confident in the credibility of this interpretation. For example, IdentityConfidence = questionable is appropriate when a geologist reasons "I can see some kind of planar feature that separates map units in this outcrop, but I cannot be certain if it is a contact or a fault."</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>certain</edomv>
                <edomvd>Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation.</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>IdentityConfidence</attrlabl>
            <attrdef>Confidence that feature is correctly identified.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>questionable</edomv>
                <edomvd>Identity of a feature cannot be determined using relevant observations and scientific judgment; therefore, one cannot be reasonably confident in the credibility of this interpretation. For example, IdentityConfidence = questionable is appropriate when a geologist reasons "I can see some kind of planar feature that separates map units in this outcrop, but I cannot be certain if it is a contact or a fault."</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>certain</edomv>
                <edomvd>Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation.</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Notes</attrlabl>
            <attrdef>Additional information specific to a particular feature or table entry.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain. Free text. Values of &lt;null&gt; or #null indicate no entry.</udom>
            </attrdomv>
          </attr>
        </detailed>
        <detailed>
          <enttyp>
            <enttypl>GeoMaterialDict</enttypl>
            <enttypd>Non-spatial table that provides values of GeoMaterial, placed in a hierarchy, and their definitions. For further information, see Appendix A in GeMS documentation, available at http://ngmdb.usgs.gov/Info/standards/GeMS.</enttypd>
            <enttypds>GeMS</enttypds>
          </enttyp>
          <attr>
            <attrlabl>OBJECTID</attrlabl>
            <attrdef>Internal feature number</attrdef>
            <attrdefs>ESRI</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>HierarchyKey</attrlabl>
            <attrdef>String that records hierarchical structure. Has form nn-nn-nn, nnn-nnn, or similar. Numeric, left-padded with zeros, dash-delimited. Each HierarchyKey fragment of each row MUST be the same length to allow text-based sorting of table entries.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>GeoMaterial</attrlabl>
            <attrdef>Categorization of map unit based on lithologic and genetic character, term selected from NGMDB standard term list defined in Appendix A of GeMS documentation, available at http://ngmdb.usgs.gov/Info/standards/GeMS..</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>Eolian sediment</edomv>
                <edomvd>Silt- and sand-sized sediment, deposited by wind.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coastal zone sediment</edomv>
                <edomvd>Mud and sand, with lesser amounts of gravel, deposited on beaches, on barrier islands, or in nearshore-marine, deltaic, or various low-energy shoreline (mud flat, tidal flat, sabka, algal flat) environments.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Metasedimentary rock</edomv>
                <edomvd>Rock derived from preexisting sedimentary rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Chert</edomv>
                <edomvd>Sedimentary rock, composed chiefly of microcrystalline or cryptocrystalline quartz.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coastal zone sediment, mostly coarse-grained</edomv>
                <edomvd>Mostly sand, silt, and gravel, deposited on beaches, in dunes, and in shallow-marine and related alluvial environments.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Igneous and metamorphic rock</edomv>
                <edomvd>Consists of coarse-grained intrusive igneous rock and generally medium- to high-grade metamorphic rock.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Meta-ultramafic rock</edomv>
                <edomvd>Rock derived from preexisting ultramafic rocks by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Composed mostly of magnesium-bearing minerals (for example, serpentine, talc, magnesite).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Debris flows, landslides, and other localized mass-movement sediment</edomv>
                <edomvd>Sediment formed by relatively localized, downslope transport of particles or clasts produced by weathering and breakdown of underlying rock, sediment, and (or) soil. Composed of poorly sorted and poorly stratified material that ranges in size from clay to boulders. Speed of downslope transport ranges from rapid to imperceptible.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Lacustrine sediment, mostly coarse-grained</edomv>
                <edomvd>Mostly well-sorted and well-bedded material, generally sand and gravel sized, with lesser amounts of silt and clay, deposited in perennial to intermittent lakes. Much of sediment is derived from material eroded and transported by streams. Mostly deposits of lake-marginal beaches and deltas.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Medium and high-grade regional metamorphic rock, of unspecified origin</edomv>
                <edomvd>Rock derived from preexisting rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to relatively intense regional changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Origin of preexisting rock is mixed (for example, igneous and sedimentary) or is not known. Includes amphibolite, granulite, schist, and gneiss.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Alluvial sediment</edomv>
                <edomvd>Unconsolidated material deposited by streams or other bodies of running water as sorted or semisorted sediment in streambed, or on its floodplain or delta, or as cone or fan at base of mountain slope. Grain size varies from clay to gravel.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Meta-volcaniclastic rock</edomv>
                <edomvd>Rock derived from preexisting volcaniclastic rocks by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Composed of deformed but recognizable particles or clasts of volcanic explosive material.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Intermediate-composition lava flows</edomv>
                <edomvd>Lateral, surficial outpourings of molten lava from vent or fissure; also, solidified bodies of rock that form when they cool. Parental magma commonly erupts from stratovolcanoes as thick lava flows. Includes rocks that are, in color and in mineral composition, intermediate between felsic and mafic rocks (for example, andesite).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Pyroclastic flows</edomv>
                <edomvd>Hot ash, pumice, and rock fragments erupted from volcano or caldera. Material moves downslope commonly in chaotic flows; once deposited, hot fragments may compact under their own weight and weld together.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Carbonate rock</edomv>
                <edomvd>Sedimentary rock, consisting chiefly of carbonate minerals such as limestone or dolomite. </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>"Made" or human-engineered land</edomv>
                <edomvd>Modern, unconsolidated material known to have human-related origin.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Playa sediment</edomv>
                <edomvd>Fine-grained clastic sediment and evaporitic salts, deposited in ephemeral lakes in centers of undrained basins. Includes material deposited in playas, mud flats, salt flats, and adjacent saline marshes. Generally interbedded with eolian sand and with lacustrine sediment deposited during wetter climatic periods; commonly intertongues upslope with sediment deposited by alluvial fans.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Unmapped area</edomv>
                <edomvd>Unmapped area</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Alluvial sediment, mostly coarse-grained</edomv>
                <edomvd>Unconsolidated material deposited by streams or other bodies of running water as sorted or semisorted sediment in streambed, or on its floodplain or delta, or as cone or fan at base of mountain slope. Sediment is mostly sand, gravel, and coarser material but may also contain some silt and clay.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Sedimentary and extrusive igneous material</edomv>
                <edomvd>Either (1) sedimentary rock and (or) unconsolidated material (sediment) and extrusive igneous material (volcanic rock and [or] sediment) or (2) volcanic rock and (or) sediment and such material after erosion and redeposition.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Metaigneous rock</edomv>
                <edomvd>Rock derived from preexisting igneous rocks and altered by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, shear stress, and (or) chemical environment, generally at depth in Earths crust. </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coarse-grained intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Meta-felsic and intermediate rock</edomv>
                <edomvd>Rock derived from preexisting felsic and intermediate-composition rocks by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Composed mostly of light-colored minerals; relatively enriched in silica. Includes metagranite, metadiorite, and meta-andesite.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Marine sediment, mostly coarse-grained</edomv>
                <edomvd>Mud, sand, and gravel eroded from rocks and sediment on land, transported by streams, and deposited in marine deltas and basins. Mostly siliceous in composition.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Dolomite</edomv>
                <edomvd>Carbonate sedimentary rock, consisting chiefly of dolomite. Although dolostone is the proper analog to limestone, it has not often been applied to dolomitic units.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Lacustrine sediment, mostly fine-grained</edomv>
                <edomvd>Mostly well-sorted and well-bedded material, generally silt and clay sized, with lesser amounts of sand, deposited in perennial to intermittent lakes. </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coal and lignite</edomv>
                <edomvd>Organic-rich sedimentary rock, formed from compaction and alteration of plant remains. Coal is consolidated, harder, black rock. Lignite is semiconsolidated, brown to black, earthy material that may contain large particles of recognizable plant parts and tends to crack upon drying.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Slate and phyllite, of sedimentary-rock origin</edomv>
                <edomvd>Fine-grained rock derived from preexisting sedimentary rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Includes phyllite and slate (compact, fine-grained rock that possesses strong cleavage and, hence, can be split into slabs and thin plates). Mostly formed from fine-grained material such as mudstone.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Air-fall tephra</edomv>
                <edomvd>Fragments of volcanic rock and lava, of various sizes, carried into air by explosions and by hot gases in eruption columns or lava fountains; known as tephra. As tephra falls to ground, with increasing distance from volcano, average size of individual rock particles and thickness of resulting deposit decrease. Fine tephra deposited at some distance from volcano is known as volcanic ash.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coastal zone sediment, mostly fine-grained</edomv>
                <edomvd>Mostly clay and silt, deposited in lagoons, tidal flats, backbarriers, and coastal marshes.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Sand and gravel of unspecified origin</edomv>
                <edomvd>Sediment composed mostly of sand and (or) gravel, formed by weathering and erosion of preexisting rocks or minerals; eroded particles or clasts are transported and deposited by gravity, air, water, or ice.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Sedimentary material</edomv>
                <edomvd>An aggregation of particles deposited by gravity, air, water, or ice, or as accumulated by other natural agents operating at Earths surface such as chemical precipitation or secretion by organisms. May include unconsolidated material (sediment) and (or) sedimentary rock. Does not include sedimentary material directly deposited as a result of volcanic activity.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Loess</edomv>
                <edomvd>Silty sediment, deposited by wind, commonly near glacial margin.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Conglomerate</edomv>
                <edomvd>Sedimentary rock, composed predominantly of particles or clasts derived by erosion and weathering of preexisting rock; contains more than 30 percent gravel-sized clasts.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Mostly mudstone</edomv>
                <edomvd>Mostly mudstone, interbedded with other sedimentary rocks that locally may include coarser grained clastic rocks (sandstone, conglomerate), carbonates, and (or) coal.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Alluvial sediment, mostly fine-grained</edomv>
                <edomvd>Unconsolidated material deposited by streams or other bodies of running water as sorted or semisorted sediment in streambed, or on its floodplain or delta, or as cone or fan at base of mountain slope. Sediment is mostly silt and clay but may also contain some sand and gravel.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Intermediate-composition pyroclastic flows</edomv>
                <edomvd>Hot ash, pumice, and rock fragments erupted from volcano. Material moves downslope commonly in chaotic flows; once deposited, hot fragments may compact under their own weight and weld together. Parental magma commonly erupts from stratovolcanoes as thick lava flows but also can generate strong explosive eruptions to form pyroclastic flows. Includes rocks that are, in color and mineral composition, intermediate between felsic and mafic rocks (for example, andesite).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Limestone</edomv>
                <edomvd>Carbonate sedimentary rock, consisting chiefly of calcite.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coarse-grained, intermediate-composition intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye. Intermediate in color and in mineral composition (between felsic and mafic igneous rock). Includes dioritic rock.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Dune sand</edomv>
                <edomvd>Mostly sand-sized sediment, deposited by wind. Typically characterized by various dune landforms.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Exotic-composition intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) below Earths surface that has exotic mineralogical, textural, or field setting characteristics. Typically dark colored with abundant phenocrysts. Includes kimberlite, lamprophyre, lamproite, and foiditic rocks.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Marine sediment</edomv>
                <edomvd>Mud and sand, deposited in various marine environments. May originate from erosion of rocks and sediment or may be derived from marine organisms (of carbonate or siliceous composition).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Ultramafic intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye. Composed almost entirely of mafic minerals (for example, hypersthene, augite, olivine).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Sedimentary rock</edomv>
                <edomvd>Consolidated material (rock) composed of particles transported and deposited by gravity, air, water, or ice, or accumulated by other natural agents operating at Earths surface, such as chemical precipitation or secretion by organisms. Does not here include sedimentary material directly deposited as result of volcanic activity.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Contact-metamorphic rock</edomv>
                <edomvd>Altered rock that originated by local processes of thermal metamorphism, genetically related to intrusion and extrusion of magmas and taking place at or near contact with body of igneous rock. Metamorphic changes are effected by heat and fluids emanating from magma and by some deformation because of emplacement of igneous mass.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Igneous rock</edomv>
                <edomvd>Rock and fragmental material that solidified from molten or partly molten material (magma). </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Lava flows</edomv>
                <edomvd>Lateral, surficial outpourings of molten lava from vent or fissure; also, solidified bodies of rock that form when they cool. Composed generally of fine-grained, dark-colored rocks (for example, basalt), which tend to form extensive sheets that have generally low relief, except in vent areas where cinder cones or shield volcanoes may form. Includes basaltic shield volcanoes, which may become very large (for example, Hawaii).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Mafic-composition pyroclastic flows</edomv>
                <edomvd>Hot ash, pumice, and rock fragments erupted from volcano. Material moves downslope commonly in chaotic flows; once deposited, hot fragments may compact under their own weight and weld together. Because of their low silica content and resulting low viscosity, parental magmas tend to erupt gently as lava flows rather than more forcefully as pyroclastic flows. Includes basalt; rocks are commonly dark-colored. </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Other materials</edomv>
                <edomvd>Other materials</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Mass movement sediment</edomv>
                <edomvd>Sediment formed by downslope transport of particles or clasts produced by weathering and breakdown of underlying rock, sediment, and (or) soil. Composed of poorly sorted and poorly stratified material that ranges in size from clay to boulders. Includes colluvial, landslide, talus, and rock-avalanche deposits.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Silt and clay of unspecified origin</edomv>
                <edomvd>Sediment composed mostly of silt and (or) clay, formed by weathering and erosion of preexisting rocks or minerals; eroded particles or clasts are transported and deposited by gravity, air, water, or ice.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Marine sediment, mostly fine-grained</edomv>
                <edomvd>Mostly clay- and silt-sized sediment, deposited in relatively deep, quiet water, far removed from areas where coarser grained clastic sediments are washed into marine environment. Includes sediment derived from marine organisms.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Evaporitic rock</edomv>
                <edomvd>Sedimentary rock, composed primarily of minerals produced by evaporation of saline solution. Examples include gypsum, anhydrite, other diverse sulfates, halite (rock salt), primary dolomite, and rocks composed of various nitrates and borates.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Glacial till</edomv>
                <edomvd>Mostly unsorted and unstratified material, generally unconsolidated, deposited directly by and underneath or adjacent to glacier without subsequent reworking by meltwater. Consists of heterogeneous mixture of clay, silt, sand, gravel, and boulders, ranging widely in size and shape.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Quartzite</edomv>
                <edomvd>Rock derived from preexisting quartz-rich sedimentary rocks (commonly sandstone) and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, shear stress, and (or) chemical environment, generally at depth in Earths crust. </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) below Earths surface.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Metamorphic rock</edomv>
                <edomvd>Rock derived from preexisting rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Volcaniclastic (fragmental) material</edomv>
                <edomvd>Rock and unconsolidated material consisting of particles or clasts that were formed by volcanic explosion or aerial expulsion from volcanic vent.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Mafic-composition lava flows</edomv>
                <edomvd>Lateral, surficial outpourings of molten lava from vent or fissure; also, solidified bodies of rock that form when they cool. Low-silica parental magmas have low viscosity and tend to form extensive sheets that have generally low relief. Includes basaltic shield volcanoes, which may become very large (for example, in Hawaii). Composed of fine-grained, dark rocks, including basaltic.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Rock and sediment</edomv>
                <edomvd>Various rocks and sediment, not differentiated.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Colluvium and other widespread mass-movement sediment</edomv>
                <edomvd>Sediment formed by slow, relatively widespread, downslope transport of particles or clasts produced by weathering and breakdown of underlying rock, sediment, and (or) soil. Composed of poorly sorted and poorly stratified material that ranges in size from clay to boulders.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Sandstone</edomv>
                <edomvd>Sedimentary rock, composed predominantly of particles or clasts derived by erosion and weathering of preexisting rock; consists mostly of sand-sized particles, with or without fine-grained matrix of silt or clay.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Fine-grained intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at shallow depth beneath Earths surface, thereby cooling quickly. Generally fine grained but may contain large mineral crystals (phenocrysts). Mostly found as tabular dikes or sills.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Ice-contact and ice-marginal sediment, mostly fine-grained</edomv>
                <edomvd>Mostly silt- and clay-sized particles or clasts, with lesser amounts of sand and gravel, derived from rock or preexisting sediment that has been eroded and transported by glaciers. As glacier melted, material was deposited by running water essentially in contact with glacial ice or was transported and deposited by glacially fed streams. Includes sediment deposited into water bodies adjacent to glacier.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Sediment</edomv>
                <edomvd>Unconsolidated material (sediment) composed of particles deposited by gravity, air, water, or ice, or as accumulated by other natural agents operating at Earths surface such as chemical precipitation or secretion by organisms. Does not include sedimentary material directly deposited as a result of volcanic activity.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Deformation-related metamorphic rock</edomv>
                <edomvd>Rock derived from preexisting rocks by essentially solid-state mineralogical, chemical, or structural changes in response to strong deformation, commonly in association with marked changes in temperature, pressure, and (or) chemical environment. Generally forms in narrow, planar zones of local deformation (for example, along faults); characterized by foliation or alignment of mineral grains. Includes mylonite and cataclasite.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Iron-rich sedimentary rock</edomv>
                <edomvd>Sedimentary rock, in which at least half (by volume) of observed minerals are iron bearing (hematite, magnetite, limonite group minerals, siderite, iron sulfides).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Felsic-composition lava flows</edomv>
                <edomvd>Lateral, surficial outpourings of molten lava from vent or fissure; also, solidified bodies of rock that form when they cool. Because of their high silica content and resulting high viscosity, parental magmas tend to erupt explosively, and so these deposits are uncommon. Includes fine-grained, light-colored rock with rhyolitic, dacitic, trachytic, and latitic composition.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Sandstone and mudstone</edomv>
                <edomvd>Sandstone and mudstone (including shale and siltstone), in approximately equal (or unspecified) proportions. </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Mafic-composition air-fall tephra</edomv>
                <edomvd>Fragments of volcanic rock and lava, of various sizes, carried into the air by explosions and by hot gases in eruption columns or lava fountains; known as tephra. As tephra falls to ground, with increasing distance from volcano, average size of individual rock particles and thickness of resulting deposit decrease. Because of their low silica content and resulting low viscosity, parental magmas tend to erupt gently as lava flows, and so these deposits are uncommon. Includes basalt; rocks are commonly dark-colored. </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Intermediate-composition air-fall tephra</edomv>
                <edomvd>Fragments of volcanic rock and lava, of various sizes, carried into the air by explosions and by hot gases in eruption columns or lava fountains; known as tephra. As tephra falls to ground, with increasing distance from volcano, average size of individual rock particles and thickness of resulting deposit decrease. Parental magma commonly erupts from stratovolcanoes as thick lava flows but also can generate strong explosive eruptions to form pyroclastic flows. Includes rocks that are, in color and mineral composition, intermediate between felsic and mafic rocks (for example, andesite). </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Residual material</edomv>
                <edomvd>Unconsolidated material, developed in place by weathering of underlying rock or sediment. Usually forms relatively thin surface layer that conceals unweathered or partly altered source material. Material from which soils are formed.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Mostly sandstone</edomv>
                <edomvd>Mostly sandstone, interbedded with other sedimentary rocks that locally may include conglomerate and finer grained clastic rocks (mudstone), carbonates, and (or) coal.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Clastic sediment</edomv>
                <edomvd>Sediment formed by weathering and erosion of preexisting rocks or minerals; eroded particles or clasts are transported and deposited by gravity, air, water, or ice.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Water or ice</edomv>
                <edomvd>Water or ice</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Ice-contact and ice-marginal sediment</edomv>
                <edomvd>Mostly sand-, silt-, and gravel-sized particles or clasts derived from rock or preexisting sediment that has been eroded and transported by glaciers. As glacier melted, material was deposited by running water essentially in contact with glacial ice or was transported and deposited by glacially fed streams. Includes sediment deposited into water bodies adjacent to glacier.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Felsic-composition pyroclastic flows</edomv>
                <edomvd>Hot ash, pumice, and rock fragments erupted from volcano or caldera. Material moves downslope commonly in chaotic flows; once deposited, hot fragments may compact under their own weight and weld together. Because of their high-silica content and resulting high viscosity, parental magmas tend to erupt explosively. Includes rhyolite, dacite, trachyte, latite; rocks are commonly light-colored.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Fine-grained, intermediate-composition intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at shallow depth beneath Earths surface, thereby cooling quickly. Generally fine grained but may contain large mineral crystals (phenocrysts). Mostly found as tabular dikes or sills. Intermediate in color and in mineral composition (between felsic and mafic igneous rock). Includes andesitic rock.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Mostly carbonate rock</edomv>
                <edomvd>Mostly carbonate rock, interbedded with other sedimentary rock types.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Regional metamorphic rock, of unspecified origin</edomv>
                <edomvd>Rock derived from preexisting rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked regional changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Origin of preexisting rock is mixed (for example, igneous and sedimentary) or is not known. </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Glacial till, mostly silty</edomv>
                <edomvd>Mostly unsorted and unstratified material, generally unconsolidated, deposited directly by and underneath or adjacent to glacier without subsequent reworking by meltwater. Consists of heterogeneous mixture of clay, silt, sand, gravel, and boulders, ranging widely in size and shape. Relatively loamy (silty) in texture.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Mudstone</edomv>
                <edomvd>Sedimentary rock, composed predominantly of particles or clasts derived by erosion and weathering of preexisting rock; consists mostly of mud (that is, silt- and clay-sized particles). Includes shale and siltstone.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Lower-grade metamorphic rock, of unspecified origin</edomv>
                <edomvd>Rock derived from preexisting rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to relatively mild regional changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Origin of preexisting rock is mixed (for example, igneous and sedimentary) or is not known. Includes slate and phyllite.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Carbonate sediment</edomv>
                <edomvd>Sediment formed by biotic or abiotic precipitation from aqueous solution of carbonates of calcium, magnesium, or iron (for example, limestone, dolomite).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Fine-grained, felsic-composition intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at shallow depth beneath Earths surface, thereby cooling quickly. Generally fine grained but may contain large mineral crystals (phenocrysts). Mostly found as tabular dikes or sills. Composed mostly of light-colored minerals. Includes rhyolitic, dacitic, trachytic, and latitic rock.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Rock</edomv>
                <edomvd>Various rock types, not differentiated.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Meta-carbonate rock</edomv>
                <edomvd>Rock derived from preexisting carbonate sedimentary rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Characterized by recrystallization of carbonate minerals in source rock. Includes marble (for which preexisting rock was dominantly limestone or other rock composed of calcite), dolomitic marble, meta-dolostone, and meta-dolomite (for which preexisting rock contained appreciable amount of magnesium).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Peat and muck</edomv>
                <edomvd>Unconsolidated material, principally composed of plant remains, with lesser amounts of fine-grained clastic sediment. Deposited in water-saturated environment such as swamp, marsh, or bog. With lithification, such material becomes coal.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Felsic-composition air-fall tephra</edomv>
                <edomvd>Fragments of volcanic rock and lava, of various sizes, carried into air by explosions and by hot gases in eruption columns or lava fountains; known as tephra. As tephra falls to ground, with increasing distance from volcano, average size of individual rock particles and thickness of resulting deposit decrease. Because of their high silica content and resulting high viscosity, felsic-composition magmas tend to erupt explosively, readily forming pumice and volcanic ash. Composed of light-colored rocks (for example, rhyolite, dacite, trachyte, latite). </edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Schist and gneiss, of sedimentary-rock origin</edomv>
                <edomvd>Foliated rock derived from preexisting sedimentary rocks by essentially solid-state mineralogical, chemical, or structural changes in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Includes schist (characterized by such strong foliation or alignment of minerals that it readily splits into flakes or slabs) and gneiss (characterized by alternating, irregular bands of different mineral composition). Mostly formed from fine-grained material such as mudstone.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Glacial till, mostly clayey</edomv>
                <edomvd>Mostly unsorted and unstratified material, generally unconsolidated, deposited directly by and underneath or adjacent to glacier without subsequent reworking by meltwater. Consists of heterogeneous mixture of clay, silt, sand, gravel, and boulders, ranging widely in size and shape. Relatively clayey in texture.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coarse-grained, mafic-composition intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye. Composed mostly of feldspar and dark-colored minerals. Includes gabbroic rock.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Clastic sedimentary rock</edomv>
                <edomvd>Sedimentary rock, composed predominantly of particles or clasts derived by erosion, weathering, or mass-wasting of preexisting rock and deposited by gravity, air, water, or ice.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Volcanic mass flow</edomv>
                <edomvd>Volcanic deposits formed by mass movement (for example, debris avalanches, debris flows, lahar deposits), in many cases triggered by volcanic eruption. Debris avalanches that occur on volcanoes clearly without eruptive trigger may be classified as sedimentary (for example, as Debris flows, landslides, and other localized mass-movement sediment).</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Coarse-grained, felsic-composition intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye. Composed mostly of light-colored minerals (for example, feldspar, quartz). Includes granitic, syenitic, and monzonitic rock.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Meta-mafic rock</edomv>
                <edomvd>Rock derived from preexisting mafic rocks by essentially solid-state, mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Composed mostly of iron- and magnesium-bearing, dark-colored and (or) green minerals. Includes greenstone, amphibolite, and metagabbro.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Lacustrine sediment</edomv>
                <edomvd>Mostly well-sorted and well-bedded material that ranges in grain size from clay to gravel, deposited in perennial to intermittent lakes. Much of sediment is derived from material eroded and transported by streams. Includes deposits of lake-marginal beaches and deltas.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Glacial till, mostly sandy</edomv>
                <edomvd>Mostly unsorted and unstratified material, generally unconsolidated, deposited directly by and underneath or adjacent to glacier without subsequent reworking by meltwater. Consists of heterogeneous mixture of clay, silt, sand, gravel, and boulders, ranging widely in size and shape. Relatively sandy in texture.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Fine-grained, mafic-composition intrusive igneous rock</edomv>
                <edomvd>Rock that solidified from molten or partly molten material (magma) at shallow depth beneath Earths surface, thereby cooling quickly. Generally fine grained but may contain large mineral crystals (phenocrysts). Mostly found as tabular dikes or sills. Composed mostly of dark-colored minerals. Includes basaltic rock.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Ice-contact and ice-marginal sediment, mostly coarse-grained</edomv>
                <edomvd>Mostly sand- and gravel-sized particles or clasts, with lesser amounts of silt and clay, derived from rock or preexisting sediment that has been eroded and transported by glaciers. As glacier melted, material was deposited by running water essentially in contact with glacial ice or was transported and deposited by glacially fed streams. Includes sediment deposited into water bodies adjacent to glacier.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Extrusive igneous material</edomv>
                <edomvd>Molten material that was erupted onto Earths surface, fusing into rock or remaining as unconsolidated particles. Includes pyroclastic flows, air-fall tephra, lava flows, and volcanic mass flows.</edomvd>
                <edomvds>GeMS</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>IndentedName</attrlabl>
            <attrdef>Name with addition of leading spaces to help show rank within a hierarchical list.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Definition</attrlabl>
            <attrdef>Plain-language definition.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
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        </detailed>
        <detailed>
          <enttyp>
            <enttypl>MapUnitPolys</enttypl>
            <enttypd>Polygons that record distribution of map units (including water, snowfields, glaciers, and unmapped area) on the particular map horizon.  In the original file geodatabase, this dataset is found within the GeologicMap feature dataset.</enttypd>
            <enttypds>GeMS</enttypds>
          </enttyp>
          <attr>
            <attrlabl>OBJECTID</attrlabl>
            <attrdef>Internal feature number</attrdef>
            <attrdefs>ESRI</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Shape</attrlabl>
            <attrdef>Internal geometry object</attrdef>
            <attrdefs>ESRI</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Shape_Length</attrlabl>
            <attrdef>Internal feature length, double</attrdef>
            <attrdefs>ESRI</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Shape_Area</attrlabl>
            <attrdef>Internal feature area, double</attrdef>
            <attrdefs>ESRI</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>MapUnit</attrlabl>
            <attrdef>Short plain-text identifier of the map unit. Foreign key to DescriptionOfMapUnits table.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>Ygg</edomv>
                <edomvd>Granitic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>pC</edomv>
                <edomvd>Undifferentiated Precambrian rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Aum</edomv>
                <edomvd>Ultramafic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Ai</edomv>
                <edomvd>Intrusive rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>PZpCm</edomv>
                <edomvd>Metamorphic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Ymc</edomv>
                <edomvd>Carbonate and meta-carbonate rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>PZpCu</edomv>
                <edomvd>Undifferentiated Paleozoic to Precambrian rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Zu</edomv>
                <edomvd>Undifferentiated Neoproterozoic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Zm</edomv>
                <edomvd>Metamorphic and igneous rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>Xu</edomv>
                <edomvd>Undifferentiated Paleoproterozoic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Ymss</edomv>
                <edomvd>Clastic sedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Au</edomv>
                <edomvd>Undifferentiated Archean rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Xif</edomv>
                <edomvd>Iron formation</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Aig</edomv>
                <edomvd>Granitic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Yms</edomv>
                <edomvd>Sedimentary and metasedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Ymg</edomv>
                <edomvd>Mafic intrusive rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Xim</edomv>
                <edomvd>Gabbro and mafic lava flows</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>PRu</edomv>
                <edomvd>Undifferentiated Proterozoic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>CAZms</edomv>
                <edomvd>Metasedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>water</edomv>
                <edomvd>Water and ice</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Xmsq</edomv>
                <edomvd>Quartzite</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Zg</edomv>
                <edomvd>Granitic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>af</edomv>
                <edomvd>Artificial fill</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Xi</edomv>
                <edomvd>Igneous and metaigneous rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>unmapped</edomv>
                <edomvd>Unmapped areas</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Yl</edomv>
                <edomvd>Igneous rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>PHs</edomv>
                <edomvd>Phanerozoic cover rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Zms</edomv>
                <edomvd>Metasedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>PZpCg</edomv>
                <edomvd>Igneous rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Ams</edomv>
                <edomvd>Metasedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>PZpCms</edomv>
                <edomvd>Metasedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>scz</edomv>
                <edomvd>Shear zone rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Zmg</edomv>
                <edomvd>Metaigneous rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Xig</edomv>
                <edomvd>Granitic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Yu</edomv>
                <edomvd>Undifferentiated Mesoproterozoic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>PRum</edomv>
                <edomvd>Ultramafic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Xms</edomv>
                <edomvd>Metasedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>PHi</edomv>
                <edomvd>Phanerozoic igneous rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>PZpCmg</edomv>
                <edomvd>Metaigneous rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Xmss</edomv>
                <edomvd>Slate and sandstone</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>PZpCum</edomv>
                <edomvd>Ultramafic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Aif</edomv>
                <edomvd>Iron formation</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Zs</edomv>
                <edomvd>Clastic sedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>IdentityConfidence</attrlabl>
            <attrdef>Confidence that feature is correctly identified.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>questionable</edomv>
                <edomvd>Identity of a feature cannot be determined using relevant observations and scientific judgment; therefore, one cannot be reasonably confident in the credibility of this interpretation. For example, IdentityConfidence = questionable is appropriate when a geologist reasons "I can see some kind of planar feature that separates map units in this outcrop, but I cannot be certain if it is a contact or a fault."</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>certain</edomv>
                <edomvd>Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation.</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Label</attrlabl>
            <attrdef>Plain-text equivalent of the desired annotation for a feature: for example "14 Ma", or "^c" which (when used with the FGDC GeoAge font) results in the geologic map-unit label TRc (with TR run together to make the Triassic symbol).</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Symbol</attrlabl>
            <attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>DataSourceID</attrlabl>
            <attrdef>Source of data; foreign key to table DataSources.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>1032</edomv>
                <edomvd>Haley, B.R., Glick, E.E., Bush, W.V., Clardy, B.F., Stone, C.G., Woodward, M.B., and Zachry, D.L., 1993, Geologic map of Arkansas: U.S. Geological Survey, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>674</edomv>
                <edomvd>Mudrey Jr., M.G., Brown, B.A., Greenberg, J.K., 1982, Bedrock Geologic Map of Wisconsin: Wisconsin Geological and Natural History Survey Map M-078, scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>955</edomv>
                <edomvd>Zen, E-an, Goldsmith, R., Ratcliffe, N.M., Robinson, P., Stanley, R.S., Hatch, N.L., Shride, A.F., Weed, E.G.A., and Wones, D.R., 1983, Bedrock geologic map of Massachusetts: U.S. Geological Survey, 3 sheets, scale 1:250,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1426</edomv>
                <edomvd>Evans, K.V ., and Green, G.N., 2003, Geologic map of the Salmon National Forest and vicinity, east-central Idaho: U.S. Geological Survey Geologic Investigations Series I-2765, 1 sheet, scale: 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>879</edomv>
                <edomvd>Spoljaric, N. and Jordan, R.R., 1966, Generalized geologic map of Delaware: Delaware Geological Survey, Special Publication 4, scale 1:297,500.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>602</edomv>
                <edomvd>Dalton, Richard F., Monteverde, Donald H., Sugarman, Peter J., and Volkert, Richard A., compilers. Bedrock Geologic Map of New Jersey 2014. New Jersey Geological and Water Survey. 2014, Scale 1:250,000, 5 cross-sections.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1504</edomv>
                <edomvd>Harrison, J.E., Griggs, A.B., and Wells, J.D., 1986, Geologic and structure maps of the Wallace 1 x 2 degree quadrangle, Montana and Idaho: U.S. Geological Survey Miscellaneous Investigations  Map I-1509-A, 2 sheets, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>838</edomv>
                <edomvd>New Mexico Bureau of Geology and Mineral Resources, 2003, Geologic map of New Mexico: New Mexico Bureau of Geology and Mineral Resources Geologic Map, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>921</edomv>
                <edomvd>Caldwell, D.H., Erwin, R.B., and Woodward, H.P., 1968, Geologic Map of West Virginia: West Virginia Geological and Economic Survey Map 1, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>985</edomv>
                <edomvd>Sims, P.K., Peterman, Z.E., Hildebrand, T.G., and Mahan, S., 1991, Precambrian basement map of the trans-Hudson orogen and adjacent terranes, northern Great Plains, USA: U.S. Geological Survey Miscellaneous Investigations Map I-2214, scale 1:1,000,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>856</edomv>
                <edomvd>Heran, W.D., Green, G.N., and Stoeser, D.B., A digital geologic map database for Oklahoma: U.S. Geological Survey Open-File Report 03-247, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1430</edomv>
                <edomvd>Vuke, S.M., Lonn, J.D., Berg, R.B., and Schmidt, C.J., 2014, Geologic map of the Bozeman 30' x 60' quadrangle, southwestern Montana: Montana Bureau of Mines and Geology Open-File Report 648, 44 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>591</edomv>
                <edomvd>Burchett, R.R., 1986, Geologic bedrock map of Nebraska: Nebraska Conservation and Survey Division Geologic Maps and Charts 1, scale 1:1000,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1473</edomv>
                <edomvd>Berg, R.B., Lopez, D.A., and Lonn, J.D., 2000, Geologic map of the Livingston 30' x 60' quadrangle, south-central Montana: Montana Bureau of Mines and Geology Open-File Report 406, 21 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>652</edomv>
                <edomvd>Horton, J.W., Jr., and Dicken, C.L., 2000, Preliminary geologic map of the Appalachian Piedmont and Blue Ridge, South Carolina segment: U.S. Geological Survey Open-File Report 01-298, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>799</edomv>
                <edomvd>Sims, P.K., Lund, K., Anderson, E., 2005, Precambrian Crystalline Basement Map of Idaho - An Interpreatation of Aeromagnetic Anomalies: U.S. Geological Survey Scientific Investigation Map 2884, Scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1020</edomv>
                <edomvd>Richard, S.M., Reynolds, S.J., Spencer, J.E., and Pearthree, P.A., 2000, Geologic Map of Arizona: Arizona Geological Survey, Map 35, scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1447</edomv>
                <edomvd>McDonald, C., Mosolf, J.G., Vuke, S.M., and Lonn, J.D., 2020, Geologic map of the Elliston 30? x 60? quadrangle, west-central Montana: Montana Bureau of Mines and Geology Geologic Map 77, 34 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1516</edomv>
                <edomvd>Harrison, J.E., Cressman, E.R., and Whipple, J.W., 1992, Geologic and structure maps of the Kalispell 1 x 2 degree quadrangle, Montana, and Alberta and British Columbia: U.S. Geological Survey  Miscellaneous Geologic Investigations Map 2267, 2 sheets, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1501</edomv>
                <edomvd>Harrison, J.E., Whipple, J.W., and Lidke, D.J., 1998, Geologic map of the western part of the Cut Bank 1 x 2 degree quadrangle, northwestern Montana: U.S. Geological Survey Miscellaneous Geologic Investigations Map 2593, 1 sheet, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>970</edomv>
                <edomvd>Milstein, R.L. compiler, 1987, Bedrock geology of southern Michigan: Michigan Department of Natural Resources Geological Publication BG-01, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1429</edomv>
                <edomvd>Miller, F.K., and Burmester, R.F., 2004, Geologic map of the Bonner's Ferry 30' X 60' quadrangle, Idaho and Montana: U.S. Geological Survey Miscellaneous Field Studies Map MP-2426, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>882</edomv>
                <edomvd>U.S. Geological Survey, 2014, USGS Small-scale Dataset - 1:1,000,000-Scale Coastline of the United States 201403 Shapefile: U.S. Geological Survey Data Release, https://www.sciencebase.gov/catalog/item/581d051de4b08da350d523be.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1102</edomv>
                <edomvd>Hardeman, W.D., Miller, R.A., and Swingle, G.D., 1966, Geologic Map of Tennessee: Tennessee Division of Geology State Geologic Map, scale 1:250,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>1487</edomv>
                <edomvd>Harrison, J.E., Griggs, A.B., and Wells, J.D., 1986, Geologic and structure maps of the Wallace 1 x 2 degree quadrangle, Montana and Idaho: U.S. Geological Survey Miscellaneous Investigations Map I-1509-A, 2 sheets, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1113</edomv>
                <edomvd>Barnes, V.E. (project supervisor), Hartmann, B.A., and Scranton, D.F. (cartography), 1992, Geologic Map of Texas: The University of Texas at Austin, Texas Bureau of Economic Geology, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>812</edomv>
                <edomvd>Sims, P.K., 1990, Precambrian basement map of the northern Midcontinent, U.S.A.: U.S. Geological Survey, Miscellaneous Investigations Series Map I-1853-A, scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>621</edomv>
                <edomvd>Bluemle, J.P., 1983, Geologic and topographic bedrock map of North Dakota: North Dakota Geological Survey Miscellaneous Map 25, scale 1:670,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>1467</edomv>
                <edomvd>Harrison, J.E., Cressman, E.R., and Whipple, J.W., 1992, Geologic and structure maps of Kalispell 1 x 2 degree quadrangle, Montana and Alberta, British Columbia: United States Geological Survey USGS Miscellaneous Geologic Investigation 2267, 2 sheets, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>644</edomv>
                <edomvd>Hermes, O.D., Gromet, L.P., Murray, D.P., Hamidzada, N.A., Skehan, J.W., and Mosher, S., 1994, Bedrock geologic map of Rhode Island: Rhode Island Geological Survey Rhode Island Map Series Map 1, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>946</edomv>
                <edomvd>Osberg, P.H., Hussey, A.M. and Boone, G.M., 1985, Bedrock geologic map of Maine: Maine Geological Survey, Geologic Map Series BGMM, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>1505</edomv>
                <edomvd>Reynolds, M.W., and Brandt, T.R., 2006, Preliminary geologic map of the Townsend 30' x 60' quadrangle, Montana: U.S. Geological Survey Open-File Report 2006-1138, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>935</edomv>
                <edomvd>Gray, H.H., Ault, C.H., and Keller, S.J., 1987, Bedrock geologic map of Indiana: Indiana Geological Survey Miscellaneous Map 48, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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              <edom>
                <edomv>1010</edomv>
                <edomvd>Sims, P.K., Finn, C.A., and Rystrom, V.L., 2001, USGS Open-File Report 01-199: Preliminary Precambrian Basement Map Showing Geologic-Geophysical Domains, Wyoming: U.S. Geological Survey, scale 1:1,000,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1419</edomv>
                <edomvd>Digital database of the Montana state geologic map, submitted to STATEMAP in GeMS</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
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                <edomv>1445</edomv>
                <edomvd>Skipp, Betty, Janecke, S.U., 2004, Geologic map of the Montana part of the Dubois 30' x 60' quadrangle, southwest Montana: Montana Bureau of Mines and Geology Open-File Report 490, 12 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>1091</edomv>
                <edomvd>Thompson, D.E., 2011, Geologic Map of Mississippi; after Bickler, A.R., 1969, Geologic Map of Mississippi: Mississippi Department of Environmental Quality, Office of Geology, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>1408</edomv>
                <edomvd>Walker, G.W., and MacLeod, N.S., 1991, Geologic map of Oregon: U.S. Geological Survey, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>1482</edomv>
                <edomvd>Berg, R.B., and Lonn, J.D., 1996, Preliminary geologic map of the Nez Perce Pass 30' x 60' quadrangle, Montana: Montana Bureau of Mines and Geology Open-File Report 339, 9 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>1458</edomv>
                <edomvd>Lonn, J.D., and Berg, R.B., 1996, Geologic map of the Hamilton 30' x 60' quadrangle, western Montana: Montana Bureau of Mines and Geology Open-File Report 340, 8 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1055</edomv>
                <edomvd>Lawton, D.E., Moye, F.J., Murray, J.B., O'Connor, B.J., Penley, H.M., Sandrock, G.S., Marsalis, W.E., Friddell, M.S., Hetrick, J.H., Huddlestun, P.F., Hunter, R.E., Mann, W.R., Martin, B.F., Pickering, S.M., Schneeberger, F.J., and Wilson, J.D., 1976, Geologic map of Georgia: Georgia Geological Survey, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>1514</edomv>
                <edomvd>Ruppel, E.T., O'Neill, J.M., and Lopez, D.A., 1993, Geologic map of the Dillon 1 x 2 degree quadrangle, Montana and Idaho: U.S. Geological Survey Miscellaneous Geologic Investigations Map 1803-H, 1 sheet, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>874</edomv>
                <edomvd>Rodgers, John, 1985, Bedrock geological map of Connecticut: Connecticut Geological and Natural History Survey, Department of Environmental Protection, 2 sheets, scale 1:125,000.</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>597</edomv>
                <edomvd>U.S. Geological Survey, 2014, USGS Small-scale Dataset - 1:1,000,000-Scale Coastline of the United States 201403 Shapefile: U.S. Geological Survey Data Release, https://www.sciencebase.gov/catalog/item/581d051de4b08da350d523be.</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>598</edomv>
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              <edom>
                <edomv>1489</edomv>
                <edomvd>Lopez, D.A., 2001, Preliminary geologic map of the Red Lodge 30' x 60' quadrangle, south-central Montana: Montana Bureau of Mines and Geology Open-File Report 423, 17 p., 1 sheet.</edomvd>
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              </edom>
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                <edomv>1433</edomv>
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            <attrdomv>
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                <edomv>1448</edomv>
                <edomvd>Kellogg, K.S., and Williams, V.S., 2006, Geologic map of the Ennis 30' x 60' quadrangle, Madison and Gallatin counties, Montana, and Park County, Wyoming: Montana Bureau of Mines and Geology Open-File Report 529, 27 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>896</edomv>
                <edomvd>Hintze, L.F., 1980, Geologic map of Utah: Utah Geological and Mineral Survey, Map A-1, scale 1:500,000.</edomvd>
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            <attrdomv>
              <edom>
                <edomv>1469</edomv>
                <edomvd>Ruppel, E.T., 1998, Geologic map of the eastern part of the Leadore 30' x 60' quadrangle, Montana and Idaho: Montana Bureau of Mines and Geology Open-File Report 372, 9 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
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                <edomv>1645</edomv>
                <edomvd>Osborne, W.E., Szabo, M.W., Copeland Jr., C.W., and Neathery, T.L., 1989, Geologic Map of Alabama: Geological Survey of Alabama Special Map 221, scale 1:500,000.</edomvd>
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              <edom>
                <edomv>1632</edomv>
                <edomvd>Schuster, J.E., 2005, Geologic map of Washington State: Washington Division of Geology and Earth Resources, Geologic Map GM-53, scale 1:500,000.</edomvd>
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            <attrdomv>
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                <edomv>1655</edomv>
                <edomvd>Cleaves, E.T., Edwards, J., Glaser, J.D., 1968, Geologic Map of Maryland: Maryland Geological Survey, Scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>835</edomv>
                <edomvd>Stewart, J.H, and Carlson, J.E., 1978, Geologic Map of Nevada: U.S. Geological Survey, scale 1:500,000</edomvd>
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            <attrdomv>
              <edom>
                <edomv>962</edomv>
                <edomvd>Reed, R.C., and Daniels, J., compilers., 1987, Bedrock geology of northern Michigan: Michigan Department of Natural Resources, Geological Survey Division, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>1509</edomv>
                <edomvd>Harrison, J.E., Cressman, E.R., and Whipple, J.W., 1992, Geologic and structure maps of the Kalispell 1 x 2 degree quadrangle, Montana, and Alberta and British Columbia: U.S. Geological Survey  Miscellaneous Geologic Investigations Map 2267, 2 sheets, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>632</edomv>
                <edomvd>Berg, T.M., Edmunds, W.E., Geyer, A.R., Glover, A.D., Hoskins, D.M., MacLachlan, D.B., Root, S.I., Sevon, W.D., and Socolow, A.A. 1980, Geologic map of Pennsylvania: Pennsylvania Geological Survey Map 1, Scale 1:250,000.</edomvd>
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                <edomv>1666</edomv>
                <edomvd>Jennings, C.W., Gutierrez, C., Bryant, W., Saucedo, G., and Wills, C., 2010, Geologic Map of California: California Geological Survey Geologic Data Map GDM-2.2010</edomvd>
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                <edomv>871</edomv>
                <edomvd>Love, J.D., and Christiansen, A.C., 1985, Geologic map of Wyoming: U.S. Geological Survey, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1423</edomv>
                <edomvd>Vuke, S.M., Berg, R.B., Colton, R.B., and O'Brien, H.E., 2002, Geologic map of the Belt 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 450, 19 p., 2 sheets, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
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                <edomv>1471</edomv>
                <edomvd>Harrison, J.E., Cressman, E.R., and Whipple, J.W., 1992, Geologic and structure maps of the Kalispell 1 x 2 degree quadrangle, Montana, and Alberta and British Columbia: U.S. Geological Survey  Miscellaneous Geologic Investigations Map 2267, 2 sheets, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
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                <edomv>1046</edomv>
                <edomvd>Scott, T.M., Campbell, K.M., Rupert, F.R., Arthur, J.D., Green, R.C., Means, G.H., Missimer, T.M., Lloyd, J.M., Yon, J.W. and Duncan, J.G., 2001, Geologic map of the state of Florida: Florida Geological Survey, Map Series 146, scale 1:1,000,000 (revised 2006).</edomvd>
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                <edomv>1491</edomv>
                <edomvd>McDonald, C., Lopez, D.A., Berg, R.B., and Gibson, R.I., 2005, Preliminary geologic map of the Ringling 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 511, 27 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
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                <edomv>1463</edomv>
                <edomvd>O'Neill, J.M., and Christiansen, R.L., 2002, Geologic map of the Hebgen Lake 30' x 60' quadrangle, Beaverhead, Madison, and Gallatin counties, Montana, Park and Teton counties, Wyoming, and Clark and Fremont Counties, Idaho: Montana Bureau of Mines and Geology Open-File Report 464, 21 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
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                <edomv>623</edomv>
                <edomvd>Slucher, E.R., Swinford, E.M., Larsen, G.E., Schumacher, G.A., Shrake, D.L., Rice, C.L., Caudill, M.R., Rea, R.G., and Powers, D.M., 2006, Bedrock geologic map of Ohio: Ohio Division of Geological Survey, Map BG-1, scale 1:500,000.</edomvd>
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            <attrdomv>
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                <edomv>1073</edomv>
                <edomvd>Noger, M.C., 1988, Geologic map of Kentucky: U.S. Geological Survey, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
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                <edomv>614</edomv>
                <edomvd>Rickard, L.V., Isachsen, Y.W., and Fisher, D.W., 1970, Geologic Map of New York: New York State Museum and Science Service Map and Chart Series 15 (Explanatory sheet published in 1971), 5 sheets, scale 1:250,000</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>999</edomv>
                <edomvd>Sims, P.K., 1992, Geologic map of Precambrian rocks, southern Lake Superior region, Wisconsin and northern Michigan: U.S. Geological Survey Miscellaneous Investigations Series Map I-2185, scale: 1:500,000</edomvd>
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              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>666</edomv>
                <edomvd>Ratcliffe, N.M., Stanley, R.S., Gale, M.H., Thompson, P.J., Walsh, G.J., Hatch, N.L., Rankin, D.W., Doolan, B.L., Kim, Jonathan, Mehrtens, C.J., Aleinikoff, J.N., McHone, J.G., and Masonic, L.M., 2011, Bedrock Geologic Map of Vermont: U.S. Geological Survey Scientific Investigations Map SIM-3184, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>1443</edomv>
                <edomvd>Ruppel, E.T., O'Neill, J.M., and Lopez, D.A., 1993, Geologic map of the Dillon 1 x 2 degree quadrangle, Montana and Idaho: U.S. Geological Survey Miscellaneous Geologic Investigations Map 1803-H, 1 sheet, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>1453</edomv>
                <edomvd>Berg, R.B., Lonn, J.D., and Locke, W.W., 1999, Geologic map of the Gardiner 30' x 60' quadrangle, south-central Montana: Montana Bureau of Mines and Geology Open-File Report 387, 11 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1496</edomv>
                <edomvd>Lewis, R.S., Burmester, R.F., Breckenridge, R.M., McFaddan, M.D., and Phillips, W.M., 2008, Preliminary geologic map of the Sandpoint 30' x 60' quadrangle, Idaho and Montana, and the Idaho part of the Chewelah 30' x 60' quadrangle: Idaho Geological Survey, Digital Web Map DWM-94, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1500</edomv>
                <edomvd>Mudge, M.R., Earhart, R.L., Whipple, J.W., and Harrison, J.E., 1983, Geologic and structure maps of the Choteau 1 x 2 degree quadrangle, northwestern Montana: Montana Bureau of Mines and Geology Montana Atlas 3-A, 2 sheets, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
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                <edomv>816</edomv>
                <edomvd>Jirsa, M.A., Boerboom, T.J., and Chandler, V.W., 2012, Geologic Map of Minnesota, Precambrian bedrock geology: Minnesota Geological Survey State Map Series S-22, scale 1:500,000.</edomvd>
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            <attrdomv>
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                <edomv>1479</edomv>
                <edomvd>Lonn, J.D., McDonald, C., Sears, J.W., and Smith, L.N., 2010, Geologic map of the Missoula East 30' x 60' quadrangle, western Montana: Montana Bureau of Mines and Geology Open-File Report 593, 2 sheets, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
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                <edomv>1095</edomv>
                <edomvd>Martin, J.E., Sawyer, J.F., Fahrenbach, M.D., Tomhave, D.W., and Schulz, L.D., 2004, Geologic map of South Dakota: South Dakota Geological Survey General Map G-10, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>908</edomv>
                <edomvd>Virginia Division of Mineral Resources, 1993, Geologic map of Virginia, Virginia Division of Mineral Resources, series unknown, 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
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            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>848</edomv>
                <edomvd>North Carolina Geological Survey, 1985, Geologic map of North Carolina: North Carolina Geological Survey General Geologic Map, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1442</edomv>
                <edomvd>Vuke, S.M., 2014, Preliminary geologic map of the Dearborn River 30' x 60' quadrangle, west-central Montana: Montana Bureau of Mines and Geology Open-File Report 649, 9 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1444</edomv>
                <edomvd>Bergantino, R.N., 2001, Geologic map of the Dodson 30' x 60' quadrangle, north-central Montana: Montana Bureau of Mines and Geology Open-File Report 439, 9 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1424</edomv>
                <edomvd>Porter, K.W., Wilde, E.M., and Vuke, S.M., 1996, Preliminary geologic map of the Big Snowy Mountains 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 341, 16 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1517</edomv>
                <edomvd>Porter, K.W., and Wilde, E.M., 2001, Geologic map of the Zortman 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 438, 16 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>940</edomv>
                <edomvd>Witzke, B.J., Anderson, R.R., and Pope, J.P., 2010, Bedrock Geologic Map of Iowa: Iowa Geological Survey Open-File Map OFM-2010-01, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>655</edomv>
                <edomvd>Tomhave, D.W., and Schulz, L.D., 2004, Bedrock geologic map showing configuration of the bedrock surface in South Dakota east of the Missouri River: South Dakota Geological Survey General Map 9, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>783</edomv>
                <edomvd>Sims, P.K., Bankey, V., Finn, C.A., 2001, Preliminary Precambrian basement map of Colorado-a geologic interpretation of the aeromagnetic anomaly map: U.S. Geological Survey Open-File Report 01-364, scale 1:1,000,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1472</edomv>
                <edomvd>Lonn, J.D., Skipp, B., Ruppel, E.T., Janecke, S.U., Perry Jr., W.J., Sears, J.W., Bartholomew, M.J., Stickney, M.C., Fritz, W.J., Hurlow, H.A., and Thomas, R.C., 2000, Geologic map of the Lima 30' x 60' quadrangle, southwest Montana: Montana Bureau of Mines and Geology Open-File Report 408, 42 p., 2 sheets, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1035</edomv>
                <edomvd>Tweto, Ogden, 1979, Geologic map of Colorado: U.S. Geological Survey, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1498</edomv>
                <edomvd>Mudge, M.R., Earhart, R.L., Whipple, J.W., and Harrison, J.E., 1983, Geologic and structure maps of the Choteau 1 x 2 degree quadrangle, northwestern Montana: Montana Bureau of Mines and Geology Montana Atlas 3-A, 2 sheets, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1435</edomv>
                <edomvd>Reynolds, M.W., and Brandt, T.R., 2005, Geologic map of the Canyon Ferry Dam 30' x 60' quadrangle, west-central Montana: U.S. Geological Survey Scientific Investigations Map 2860, 32 p., 3 sheets, scale 1:100,000. .</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1507</edomv>
                <edomvd>Lonn, J.D., and McFaddan, M.D., 1999, Geologic map of the Montana part of the Wallace 30' x 60' quadrangle: Montana Bureau of Mines and Geology Open-File Report 388, 15 p., 2 sheets, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1065</edomv>
                <edomvd>Kansas Geological Survey, 2008, Surficial Geology of Kansas: Kansas Geological Survey, Map M-118, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>2</edomv>
                <edomvd>Starbuck, E.A., 2017, Geologic map of Missouri, 2017; Missouri Geological Survey, GM-02-2017, scale 1:500000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>794</edomv>
                <edomvd>Anderson, R., 2006, Geology of the Precambrian surface of Iowa and surrounding area: Iowa Geological Survey Open File Map OFM-06-7, scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1494</edomv>
                <edomvd>Lonn,J.D., Elliott, C.G., Lewis, R.S., Burmester, R.F., McFaddan, M.D., Stanford, L.R., and Jänecke, S.U., 2019, Geologic map of the Montana part of the Salmon 30' x 60' quadrangle, southwestern Montana: Montana Bureau of Mines and Geology Geologic Map 75, 28 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1084</edomv>
                <edomvd>Snead, J.I., and McCulloh, R.P., 1984, Geologic Map of Louisiana: Louisiana Geological Survey Geologic Map 5, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>887</edomv>
                <edomvd>Kolata, D.R., comp., 2005, Bedrock Geology of Illinois: Champaign, Ill., Illinois State Geological Survey, Illinois Map Series 14, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1508</edomv>
                <edomvd>Reynolds, M.W., and Brandt, T.R., 2007, Preliminary geologic map of the White Sulphur Springs 30' x 60' quadrangle, Montana: U.S. Geological Survey Open-File Report 2006-1329, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1431</edomv>
                <edomvd>Lopez, D.A., 2000, Geologic map of the Bridger 30' x 60' quadrangle, Montana: Montana Bureau of Mines and Geology Geologic Map 58, 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1474</edomv>
                <edomvd>Vuke, S.M., Wilde, E.M., Lopez, D.A., and Bergantino, R.N., 2000, Geologic map of the Lodge Grass 30' x 60' quadrangle, Montana: Montana Bureau of Mines and Geology Geologic Map 56, 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1434</edomv>
                <edomvd>McDonald, C., Elliott, C.G., Vuke, S.M., Lonn, J.D., and Berg, R.B., 2012, Geologic map of the Butte South 30' x 60' quadrangle, southwestern Montana: Montana Bureau of Mines and Geology Open-File Report 622, 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1485</edomv>
                <edomvd>Lonn, J.D., Smith, L.N., and McCulloch, R.B., 2007, Geologic map of the Plains 30' x 60' quadrangle, western Montana: Montana Bureau of Mines and Geology Open-File Report 554, 43 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1484</edomv>
                <edomvd>Lonn, J.D., McDonald, C., Lewis, R.S., Kalakay, T.J., O'Neill, J.M., Berg, R.B., and Hargrave, P., 2003, Geologic map of the Philipsburg 30' x 60' quadrangle, western Montana: Montana Bureau of Mines and Geology Open-File Report 483, 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>827</edomv>
                <edomvd>Sims, P.K., O'Neill, J.M., Bankey, V., and Anderson, E., 2004, Precambrian basement geologic map of Montana -- an interpretation of aeromagnetic anomalies: U.S. Geological Survey, Scientific Investigations Map SIM-2829, scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1464</edomv>
                <edomvd>Harrison, J.E., Whipple, J.W., and Lidke, D.J., 1998, Geologic map of the western part of the Cut Bank 1 x 2 degree quadrangle, northwestern Montana: U.S. Geological Survey Miscellaneous Geologic Investigations Map 2593, 1 sheet, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1480</edomv>
                <edomvd>Lewis, R.S., 1998, Preliminary geologic map of the Montana part of the Missoula West 30' x 60' quadrangle: Montana Bureau of Mines and Geology Open-File Report 373, 20 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>994</edomv>
                <edomvd>McCormick, K.A., 2010, Precambrian Basement Terrane of South Dakota: South Dakota Geological Survey Bulletin 41, 2 Plates, Scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1652</edomv>
                <edomvd>Lewis, R.S., Link, P.K., Stanford, L.R., and Long, S.P., 2012, Geologic map of Idaho: Idaho Geological Survey, Map M-9, scale 1:750,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Notes</attrlabl>
            <attrdef>Additional information specific to a particular feature or table entry.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain. Free text. Values of &lt;null&gt; or #null indicate no entry.</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>MapUnitPolys_ID</attrlabl>
            <attrdef>Primary key.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Arbitrary string. Values should be unique within this database.</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>MapSourceID</attrlabl>
            <attrdef>Identifies source map. Foreign key to DataSources table.</attrdef>
            <attrdefs>This Report</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Source_MapUnit</attrlabl>
            <attrdef>Short, easily understood ASCII-character identifier for the source map unit. Prefixed with a MapSourceID value (from Source_DescriptionOfMapUnits) to differentiate identically-named source map units from different source maps. Otherwise conceptually equivalent to the "MapUnit" field in the GeMS "DescriptionOfMapUnits" table.</attrdef>
            <attrdefs>This Report</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
        </detailed>
        <detailed>
          <enttyp>
            <enttypl>ContactsAndFaults</enttypl>
            <enttypd>Contacts between map units, faults that bound map units, and associated dangling faults. Includes concealed faults and contacts, waterlines, snowfield and glacier boundaries, and map boundary. In the original file geodatabase, this dataset is found within the GeologicMap feature dataset.</enttypd>
            <enttypds>GeMS</enttypds>
          </enttyp>
          <attr>
            <attrlabl>OBJECTID</attrlabl>
            <attrdef>Internal feature number</attrdef>
            <attrdefs>ESRI</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Shape</attrlabl>
            <attrdef>Internal geometry object</attrdef>
            <attrdefs>ESRI</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Shape_Length</attrlabl>
            <attrdef>Internal feature length, double</attrdef>
            <attrdefs>ESRI</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Type</attrlabl>
            <attrdef>Classifier that specifies what kind of geologic feature is represented by a database element: that a certain line within feature class ContactsAndFaults is a contact, or thrust fault, or water boundary; or that a point in GeochronPoints represents a K-Ar date.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>reverse fault</edomv>
                <edomvd>A fault on which the hanging wall has moved upward relative to the footwall. The dip of the fault is usually greater than 45°.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>caldera margin</edomv>
                <edomvd>[The margin of] a large, basin-shaped volcanic depression, more or less circular or cirquelike in form, the diameter of which is many times greater than that of the included vent or vents, no matter what the steepness of the walls or form of the floor (Williams, 1941). It is formed by collapse during an eruption.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>shoreline</edomv>
                <edomvd>A line delineating the boundary of a body of water, such as a river, lake, or the ocean</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>internal contact</edomv>
                <edomvd>A planar or irregular surface separating different portions of the same geologic map unit, such as individual landslide blocks with a mapped landslide, or separately emplaced portions of a composite plutonic unit.</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>thrust fault</edomv>
                <edomvd>A fault with a dip of 45° or less over much of its extent, on which the hanging wall has moved upward relative to the footwall.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>strike-slip fault, right lateral offset</edomv>
                <edomvd>A strike-slip fault on which the side opposite the observer has been displaced to the right.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>gradational contact</edomv>
                <edomvd>A contact defined by a gradual or continuous lithologic change from one geologic map unit to another.</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>contact</edomv>
                <edomvd>A plane or irregular surface between two types or ages of rock.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>detachment fault</edomv>
                <edomvd>A regionally extensive, gently dipping normal fault that is commonly associated with extension in a metamorphic core complex.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>normal fault</edomv>
                <edomvd>A fault in which the hanging wall has moved downward relative to the footwall. The angle of the fault is usually 45-90 degrees, and in most cases close to 60 degrees.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>oblique-slip fault, left lateral offset</edomv>
                <edomvd>A fault on which the net slip has dip slip and strike slip components, and the side opposite the observer has been displaced to the left.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>shear zone</edomv>
                <edomvd>A discrete, parallel-sided zone of localized shearing displacement, which may be recognized by sigmoidal mineral-filled veins, locally well-developed cleavage or foliation, wholesale grain-size reduction or mylonitization, or some combination of these features.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>glacial terminus</edomv>
                <edomvd>The lower margin or extremity of a glacier, referring to the maximum extent (limit) reached by the glacier.</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>overturned thrust fault</edomv>
                <edomvd>A fault with an original dip of 45° or less over much of its extent, on which the hanging wall has moved upward relative to the footwall, that has subsequently been rotated beyond perpendicular so that the primary hanging wall and footwall positioning have been reversed.</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>strike-slip fault, left lateral offset</edomv>
                <edomvd>A strike-slip fault on which the side opposite the observer has been displaced to the left.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>scratch boundary</edomv>
                <edomvd>Arbitrary, non-physical boundary between map units on a geologic map. For example, between an undivided unit and its subunits, or between different names for the same package of rocks.</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>lineament</edomv>
                <edomvd>A linear feature that has been determined from aerial photographs or remotely sensed data but not identified on the ground.</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>key bed</edomv>
                <edomvd>A well-defined, easily identifiable stratum or body of strata that has sufficiently distinctive characteristics (such as lithology or fossil content) to facilitate correlation in field mapping or subsurface work.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>fault</edomv>
                <edomvd>A discrete surface or zone of discrete surfaces separating two rock masses across which one mass has slid past the other.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>listric fault</edomv>
                <edomvd>A curved downward-flattening fault, generally concave upward. Listric faults may be characterized by normal or reverse separation, but the term is used most frequently in normal faulting and is often a characteristic of growth faults.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>low-angle normal fault</edomv>
                <edomvd>A fault in which the hanging wall has moved downward relative to the footwall. The angle of the fault is less than 45 degrees.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>oblique-slip fault, right lateral offset</edomv>
                <edomvd>A fault on which the net slip has dip slip and strike slip components, and the side opposite the observer has been displaced to the right.</edomvd>
                <edomvds>Jackson, J.A., Mehl, James P., and Neuendorf, Klaus K.E., 2007, Glossary of Geology: American Geosciences Institute, Alexandria VA, online ed.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>map boundary</edomv>
                <edomvd>The boundary of the map. In a GIS database, the line that bounds the outer extent of the polygons.</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>IsConcealed</attrlabl>
            <attrdef>Flag for contacts and faults covered by overlying map unit.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>LocationConfidenceMeters</attrlabl>
            <attrdef>Estimated half-width in meters of positional uncertainty envelope; position is relative to other features in database.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Positive real number. Value of -9, -99, or -999 indicates value is unknown.</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>ExistenceConfidence</attrlabl>
            <attrdef>Confidence that feature exists.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>questionable</edomv>
                <edomvd>Identity of a feature cannot be determined using relevant observations and scientific judgment; therefore, one cannot be reasonably confident in the credibility of this interpretation. For example, IdentityConfidence = questionable is appropriate when a geologist reasons "I can see some kind of planar feature that separates map units in this outcrop, but I cannot be certain if it is a contact or a fault."</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>certain</edomv>
                <edomvd>Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation.</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>IdentityConfidence</attrlabl>
            <attrdef>Confidence that feature is correctly identified.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>questionable</edomv>
                <edomvd>Identity of a feature cannot be determined using relevant observations and scientific judgment; therefore, one cannot be reasonably confident in the credibility of this interpretation. For example, IdentityConfidence = questionable is appropriate when a geologist reasons "I can see some kind of planar feature that separates map units in this outcrop, but I cannot be certain if it is a contact or a fault."</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>certain</edomv>
                <edomvd>Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation.</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Label</attrlabl>
            <attrdef>Plain-text equivalent of the desired annotation for a feature: for example "14 Ma", or "^c" which (when used with the FGDC GeoAge font) results in the geologic map-unit label TRc (with TR run together to make the Triassic symbol).</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Symbol</attrlabl>
            <attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>DataSourceID</attrlabl>
            <attrdef>Source of data; foreign key to table DataSources.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>1093</edomv>
                <edomvd>U.S. Geological Survey, 2014, USGS Small-scale Dataset - 1:1,000,000-Scale Coastline of the United States 201403 Shapefile: U.S. Geological Survey Data Release, https://www.sciencebase.gov/catalog/item/581d051de4b08da350d523be.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>370</edomv>
                <edomvd>Nusbaum, R.L., 1978, Bedrock geologic map of the Iron Mountain Lake 7 1/2' quadrangle, Missouri; Missouri Geological Survey, RO7813, scale 1:24000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1032</edomv>
                <edomvd>Haley, B.R., Glick, E.E., Bush, W.V., Clardy, B.F., Stone, C.G., Woodward, M.B., and Zachry, D.L., 1993, Geologic map of Arkansas: U.S. Geological Survey, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>674</edomv>
                <edomvd>Mudrey Jr., M.G., Brown, B.A., Greenberg, J.K., 1982, Bedrock Geologic Map of Wisconsin: Wisconsin Geological and Natural History Survey Map M-078, scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1426</edomv>
                <edomvd>Evans, K.V ., and Green, G.N., 2003, Geologic map of the Salmon National Forest and vicinity, east-central Idaho: U.S. Geological Survey Geologic Investigations Series I-2765, 1 sheet, scale: 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>955</edomv>
                <edomvd>Zen, E-an, Goldsmith, R., Ratcliffe, N.M., Robinson, P., Stanley, R.S., Hatch, N.L., Shride, A.F., Weed, E.G.A., and Wones, D.R., 1983, Bedrock geologic map of Massachusetts: U.S. Geological Survey, 3 sheets, scale 1:250,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>650</edomv>
                <edomvd>U.S. Geological Survey, 2014, USGS Small-scale Dataset - 1:1,000,000-Scale Coastline of the United States 201403 Shapefile: U.S. Geological Survey Data Release, https://www.sciencebase.gov/catalog/item/581d051de4b08da350d523be.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>879</edomv>
                <edomvd>Spoljaric, N. and Jordan, R.R., 1966, Generalized geologic map of Delaware: Delaware Geological Survey, Special Publication 4, scale 1:297,500.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>602</edomv>
                <edomvd>Dalton, Richard F., Monteverde, Donald H., Sugarman, Peter J., and Volkert, Richard A., compilers. Bedrock Geologic Map of New Jersey 2014. New Jersey Geological and Water Survey. 2014, Scale 1:250,000, 5 cross-sections.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1504</edomv>
                <edomvd>Harrison, J.E., Griggs, A.B., and Wells, J.D., 1986, Geologic and structure maps of the Wallace 1 x 2 degree quadrangle, Montana and Idaho: U.S. Geological Survey Miscellaneous Investigations  Map I-1509-A, 2 sheets, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>838</edomv>
                <edomvd>New Mexico Bureau of Geology and Mineral Resources, 2003, Geologic map of New Mexico: New Mexico Bureau of Geology and Mineral Resources Geologic Map, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>346</edomv>
                <edomvd>Sides, J.R., 1983, Geologic map of exposed Precambrian rocks in the Lake Killarney quadrangle, Missouri [7.5]; Missouri Geological Survey, Open-File Map, OFM-83-162-MR, scale 1:24000. | Pratt, W.P., Middendorf, M.A., Satterfield, I.R., and Gerdemann, P.E., 1992, Geologic map of the Rolla 1° X 2° quadrangle, Missouri [color]; United States Geological Survey, Miscellaneous Investigations Series Map, USGS I-1998, scale 1:250000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>921</edomv>
                <edomvd>Caldwell, D.H., Erwin, R.B., and Woodward, H.P., 1968, Geologic Map of West Virginia: West Virginia Geological and Economic Survey Map 1, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>335</edomv>
                <edomvd>Anderson, R.E., 1962, Geologic map of Precambrian igneous rocks in the Taum Sauk area, Missouri; Missouri Geological Survey, RO6203, scale 1:62500.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>985</edomv>
                <edomvd>Sims, P.K., Peterman, Z.E., Hildebrand, T.G., and Mahan, S., 1991, Precambrian basement map of the trans-Hudson orogen and adjacent terranes, northern Great Plains, USA: U.S. Geological Survey Miscellaneous Investigations Map I-2214, scale 1:1,000,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>856</edomv>
                <edomvd>Heran, W.D., Green, G.N., and Stoeser, D.B., A digital geologic map database for Oklahoma: U.S. Geological Survey Open-File Report 03-247, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1430</edomv>
                <edomvd>Vuke, S.M., Lonn, J.D., Berg, R.B., and Schmidt, C.J., 2014, Geologic map of the Bozeman 30' x 60' quadrangle, southwestern Montana: Montana Bureau of Mines and Geology Open-File Report 648, 44 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>958</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>333</edomv>
                <edomvd>Robertson, F.S., 1961, Precambrian geology of the St. Francois Mountains in the Ironton 15' quadrangle, Missouri; Missouri Geological Survey, RO6101, scale 1:62500. | McCracken, Mary H., 1971, Structural features of Missouri; Missouri Geological Survey and Water Resources, RI-049, vi+99 p., 1 pl., 11 figs.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>976</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1003</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>591</edomv>
                <edomvd>Burchett, R.R., 1986, Geologic bedrock map of Nebraska: Nebraska Conservation and Survey Division Geologic Maps and Charts 1, scale 1:1000,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1473</edomv>
                <edomvd>Berg, R.B., Lopez, D.A., and Lonn, J.D., 2000, Geologic map of the Livingston 30' x 60' quadrangle, south-central Montana: Montana Bureau of Mines and Geology Open-File Report 406, 21 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1036</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1089</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>799</edomv>
                <edomvd>Sims, P.K., Lund, K., Anderson, E., 2005, Precambrian Crystalline Basement Map of Idaho - An Interpreatation of Aeromagnetic Anomalies: U.S. Geological Survey Scientific Investigation Map 2884, Scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>652</edomv>
                <edomvd>Horton, J.W., Jr., and Dicken, C.L., 2000, Preliminary geologic map of the Appalachian Piedmont and Blue Ridge, South Carolina segment: U.S. Geological Survey Open-File Report 01-298, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>673</edomv>
                <edomvd>U.S. Geological Survey, 2014, USGS Small-scale Dataset - 1:1,000,000-Scale Coastline of the United States 201403 Shapefile: U.S. Geological Survey Data Release, https://www.sciencebase.gov/catalog/item/581d051de4b08da350d523be.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>287</edomv>
                <edomvd>Berry, A.W., Jr., 1970, Geologic map of a portion of the Taum Sauk Caldera, St. Francois Mountains, Missouri; Missouri Geological Survey, RO7001, scale 1:24000. | Robertson, C.E., 1995, Geologic map of the southeast part of the Ironton 7 1/2' quadrangle, Missouri; Missouri Geological Survey, RO9503, scale 1:24000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1020</edomv>
                <edomvd>Richard, S.M., Reynolds, S.J., Spencer, J.E., and Pearthree, P.A., 2000, Geologic Map of Arizona: Arizona Geological Survey, Map 35, scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1447</edomv>
                <edomvd>McDonald, C., Mosolf, J.G., Vuke, S.M., and Lonn, J.D., 2020, Geologic map of the Elliston 30? x 60? quadrangle, west-central Montana: Montana Bureau of Mines and Geology Geologic Map 77, 34 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1437</edomv>
                <edomvd>Berg, R.B., 2008, Geologic map of the Choteau 30' x 60' quadrangle, north central Montana: Montana Bureau of Mines and Geology Open-File Report 571, 16 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1516</edomv>
                <edomvd>Harrison, J.E., Cressman, E.R., and Whipple, J.W., 1992, Geologic and structure maps of the Kalispell 1 x 2 degree quadrangle, Montana, and Alberta and British Columbia: U.S. Geological Survey  Miscellaneous Geologic Investigations Map 2267, 2 sheets, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1501</edomv>
                <edomvd>Harrison, J.E., Whipple, J.W., and Lidke, D.J., 1998, Geologic map of the western part of the Cut Bank 1 x 2 degree quadrangle, northwestern Montana: U.S. Geological Survey Miscellaneous Geologic Investigations Map 2593, 1 sheet, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>348</edomv>
                <edomvd>Brown, V.M., 1983, Geology [of exposed Precambrian rocks] of the Des Arc NE 7 1/2' quadrangle, southeast Missouri; Missouri Geological Survey, Open-File Map, OFM-84-198-GI, scale 1:24000. | Pratt, W.P., Middendorf, M.A., Satterfield, I.R., and Gerdemann, P.E., 1992, Geologic map of the Rolla 1° X 2° quadrangle, Missouri [color]; United States Geological Survey, Miscellaneous Investigations Series Map, USGS I-1998, scale 1:250000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>970</edomv>
                <edomvd>Milstein, R.L. compiler, 1987, Bedrock geology of southern Michigan: Michigan Department of Natural Resources Geological Publication BG-01, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1429</edomv>
                <edomvd>Miller, F.K., and Burmester, R.F., 2004, Geologic map of the Bonner's Ferry 30' X 60' quadrangle, Idaho and Montana: U.S. Geological Survey Miscellaneous Field Studies Map MP-2426, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>365</edomv>
                <edomvd>Amos, D.H. and Desborough, G.A., 1970, Geologic map of parts of the Ironton and Fredericktown areas, Missouri; Missouri Geological Survey, Report of Investigations, RI-047, pl-1, RO7003, scale 1:36000. | Pratt, W.P., Middendorf, M.A., Satterfield, I.R., and Gerdemann, P.E., 1992, Geologic map of the Rolla 1° X 2° quadrangle, Missouri [color]; United States Geological Survey, Miscellaneous Investigations Series Map, USGS I-1998, scale 1:250000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>882</edomv>
                <edomvd>U.S. Geological Survey, 2014, USGS Small-scale Dataset - 1:1,000,000-Scale Coastline of the United States 201403 Shapefile: U.S. Geological Survey Data Release, https://www.sciencebase.gov/catalog/item/581d051de4b08da350d523be.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1102</edomv>
                <edomvd>Hardeman, W.D., Miller, R.A., and Swingle, G.D., 1966, Geologic Map of Tennessee: Tennessee Division of Geology State Geologic Map, scale 1:250,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>328</edomv>
                <edomvd>Stickel, J.E., Jr., 1949, Igneous geology of the Bonne Terre 15' quadrangle, Missouri; Missouri Geological Survey, RO4902, scale 1:30000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>332</edomv>
                <edomvd>Zimmerman, R.A., 1959, Geologic map of the Annapolis area, Missouri; Missouri Geological Survey, RO5913, scale 1:62500.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>200</edomv>
                <edomvd>Satterfield, I.R., 1980, Reconnaissance geologic map of the Higdon 7 1/2' quadrangle, Missouri; Missouri Geological Survey, RO8003, scale 1:24000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>372</edomv>
                <edomvd>Nusbaum, R.L., 1978, Bedrock geologic map of the Iron Mountain Lake 7 1/2' quadrangle, Missouri; Missouri Geological Survey, RO7813, scale 1:24000. | Nusbaum, R.L., 1978, [Bedrock geologic map of the Iron Mountain Lake 7.5' quadrangle, Missouri]; Missouri Geological Survey, RO7813B, scale 1:24000. | Nusbaum, Robert l., 1980, A Precambrian collapse caldera boundary in the St. Francois Mountains, southeast Missouri; University of Kansas, Master's Thesis, ii+77 p., 9 figs., 1 pl., 8 tbls., 3 apps. | Pratt, W.P., Middendorf, M.A., Satterfield, I.R., and Gerdemann, P.E., 1992, Geologic map of the Rolla 1° X 2° quadrangle, Missouri [color]; United States Geological Survey, Miscellaneous Investigations Series Map, USGS I-1998, scale 1:250000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1487</edomv>
                <edomvd>Harrison, J.E., Griggs, A.B., and Wells, J.D., 1986, Geologic and structure maps of the Wallace 1 x 2 degree quadrangle, Montana and Idaho: U.S. Geological Survey Miscellaneous Investigations Map I-1509-A, 2 sheets, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1113</edomv>
                <edomvd>Barnes, V.E. (project supervisor), Hartmann, B.A., and Scranton, D.F. (cartography), 1992, Geologic Map of Texas: The University of Texas at Austin, Texas Bureau of Economic Geology, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>812</edomv>
                <edomvd>Sims, P.K., 1990, Precambrian basement map of the northern Midcontinent, U.S.A.: U.S. Geological Survey, Miscellaneous Investigations Series Map I-1853-A, scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>621</edomv>
                <edomvd>Bluemle, J.P., 1983, Geologic and topographic bedrock map of North Dakota: North Dakota Geological Survey Miscellaneous Map 25, scale 1:670,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>611</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>286</edomv>
                <edomvd>Robertson, C.E., 1995, Geologic map of the southeast part of the Ironton 7 1/2' quadrangle, Missouri; Missouri Geological Survey, RO9503, scale 1:24000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>341</edomv>
                <edomvd>Amos, D.H. and Desborough, G.A., 1970, Geologic map of parts of the Ironton and Fredericktown areas, Missouri; Missouri Geological Survey, Report of Investigations, RI-047, pl-1, RO7003, scale 1:36000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1467</edomv>
                <edomvd>Harrison, J.E., Cressman, E.R., and Whipple, J.W., 1992, Geologic and structure maps of Kalispell 1 x 2 degree quadrangle, Montana and Alberta, British Columbia: United States Geological Survey USGS Miscellaneous Geologic Investigation 2267, 2 sheets, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>644</edomv>
                <edomvd>Hermes, O.D., Gromet, L.P., Murray, D.P., Hamidzada, N.A., Skehan, J.W., and Mosher, S., 1994, Bedrock geologic map of Rhode Island: Rhode Island Geological Survey Rhode Island Map Series Map 1, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>645</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>946</edomv>
                <edomvd>Osberg, P.H., Hussey, A.M. and Boone, G.M., 1985, Bedrock geologic map of Maine: Maine Geological Survey, Geologic Map Series BGMM, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
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                <edomvds>This report</edomvds>
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                <edomv>422</edomv>
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                <edomvd>Berry, A.W., Jr., 1970, Geologic map of a portion of the Taum Sauk Caldera, St. Francois Mountains, Missouri; Missouri Geological Survey, RO7001, scale 1:24000.</edomvd>
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              <edom>
                <edomv>935</edomv>
                <edomvd>Gray, H.H., Ault, C.H., and Keller, S.J., 1987, Bedrock geologic map of Indiana: Indiana Geological Survey Miscellaneous Map 48, scale 1:500,000</edomvd>
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                <edomv>938</edomv>
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                <edomvds>This report</edomvds>
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                <edomv>1053</edomv>
                <edomvd>U.S. Geological Survey, 2014, USGS Small-scale Dataset - 1:1,000,000-Scale Coastline of the United States 201403 Shapefile: U.S. Geological Survey Data Release, https://www.sciencebase.gov/catalog/item/581d051de4b08da350d523be.</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1010</edomv>
                <edomvd>Sims, P.K., Finn, C.A., and Rystrom, V.L., 2001, USGS Open-File Report 01-199: Preliminary Precambrian Basement Map Showing Geologic-Geophysical Domains, Wyoming: U.S. Geological Survey, scale 1:1,000,000</edomvd>
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            <attrdomv>
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                <edomv>893</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
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                <edomv>820</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
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                <edomv>1419</edomv>
                <edomvd>Digital database of the Montana state geologic map, submitted to STATEMAP in GeMS</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
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                <edomv>1406</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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                <edomv>629</edomv>
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                <edomvds>This report</edomvds>
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              <edom>
                <edomv>613</edomv>
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                <edomvds>This report</edomvds>
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                <edomv>1445</edomv>
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                <edomv>1091</edomv>
                <edomvd>Thompson, D.E., 2011, Geologic Map of Mississippi; after Bickler, A.R., 1969, Geologic Map of Mississippi: Mississippi Department of Environmental Quality, Office of Geology, scale 1:500,000.</edomvd>
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              <edom>
                <edomv>194</edomv>
                <edomvd>Satterfield, I.R., 1980, Reconnaissance geologic map of the Marquand 7 1/2' quadrangle, Missouri; Missouri Geological Survey, RO8005, scale 1:24000. | Pratt, W.P., Middendorf, M.A., Satterfield, I.R., and Gerdemann, P.E., 1992, Geologic map of the Rolla 1° X 2° quadrangle, Missouri [color]; United States Geological Survey, Miscellaneous Investigations Series Map, USGS I-1998, scale 1:250000.</edomvd>
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                <edomv>1408</edomv>
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                <edomv>1482</edomv>
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                <edomvds>This report</edomvds>
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                <edomv>340</edomv>
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              <edom>
                <edomv>826</edomv>
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                <edomvds>This report</edomvds>
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                <edomv>821</edomv>
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                <edomvds>This report</edomvds>
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                <edomv>895</edomv>
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                <edomvds>This report</edomvds>
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                <edomv>1055</edomv>
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                <edomv>1098</edomv>
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                <edomvds>This report</edomvds>
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                <edomvds>This report</edomvds>
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                <edomv>975</edomv>
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                <edomv>1082</edomv>
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                <edomvds>This report</edomvds>
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              <edom>
                <edomv>894</edomv>
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                <edomvds>This report</edomvds>
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              <edom>
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              <edom>
                <edomv>798</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>920</edomv>
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                <edomvds>This report</edomvds>
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                <edomv>597</edomv>
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                <edomvds>This report</edomvds>
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                <edomv>1489</edomv>
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                <edomvds>This report</edomvds>
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                <edomv>1448</edomv>
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                <edomv>619</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>896</edomv>
                <edomvd>Hintze, L.F., 1980, Geologic map of Utah: Utah Geological and Mineral Survey, Map A-1, scale 1:500,000.</edomvd>
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                <edomv>1632</edomv>
                <edomvd>Schuster, J.E., 2005, Geologic map of Washington State: Washington Division of Geology and Earth Resources, Geologic Map GM-53, scale 1:500,000.</edomvd>
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                <edomvd>Osborne, W.E., Szabo, M.W., Copeland Jr., C.W., and Neathery, T.L., 1989, Geologic Map of Alabama: Geological Survey of Alabama Special Map 221, scale 1:500,000.</edomvd>
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                <edomv>1112</edomv>
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                <edomvds>This report</edomvds>
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                <edomvd>Cleaves, E.T., Edwards, J., Glaser, J.D., 1968, Geologic Map of Maryland: Maryland Geological Survey, Scale 1:250,000.</edomvd>
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                <edomv>997</edomv>
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                <edomvds>This report</edomvds>
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                <edomv>835</edomv>
                <edomvd>Stewart, J.H, and Carlson, J.E., 1978, Geologic Map of Nevada: U.S. Geological Survey, scale 1:500,000</edomvd>
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                <edomv>1664</edomv>
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                <edomvds>This report</edomvds>
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                <edomvd>Reed, R.C., and Daniels, J., compilers., 1987, Bedrock geology of northern Michigan: Michigan Department of Natural Resources, Geological Survey Division, scale 1:500,000.</edomvd>
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                <edomvd>Harrison, J.E., Cressman, E.R., and Whipple, J.W., 1992, Geologic and structure maps of the Kalispell 1 x 2 degree quadrangle, Montana, and Alberta and British Columbia: U.S. Geological Survey  Miscellaneous Geologic Investigations Map 2267, 2 sheets, scale 1:250,000.</edomvd>
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                <edomvd>Dake, C.L., 1929, Geologic map of Potosi-Edgehill [15'] quadrangles [Missouri]; Missouri Geological Survey, Volume, 2nd Series, V-023, scale 1:62500. | Pratt, W.P., Middendorf, M.A., Satterfield, I.R., and Gerdemann, P.E., 1992, Geologic map of the Rolla 1° X 2° quadrangle, Missouri [color]; United States Geological Survey, Miscellaneous Investigations Series Map, USGS I-1998, scale 1:250000.</edomvd>
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                <edomv>1469</edomv>
                <edomvd>Ruppel, E.T., 1998, Geologic map of the eastern part of the Leadore 30' x 60' quadrangle, Montana and Idaho: Montana Bureau of Mines and Geology Open-File Report 372, 9 p., 1 sheet, scale 1:100,000.</edomvd>
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                <edomv>568</edomv>
                <edomvd>Harrison, R.W., Orndorff, R.C., and Weary, D.J., 2002, Geologic map of the Stegall Mountain 7.5-minute quadrangle, Shannon and Carter counties, Missouri; United States Geological Survey, Geologic Investigations Series, USGS I-2767, scale 1:24000. | Weary, D.J., Harrison, R.W., Orndorff, R.C., Weems, R.E., Schindler, J.S., Repetski, J.E., and Pierce, H.A., 2015, Bedrock geologic map of the Spring Valley, West Plains, and parts of the Piedmont and Poplar Bluff 30' x 60' quadrangles, Missouri, including the upper Current River and Eleven Point River drainage basins; United States Geological Survey, Scientific Investigations Map, USGS SIM-3280, scale 1:100000.</edomvd>
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                <edomv>1423</edomv>
                <edomvd>Vuke, S.M., Berg, R.B., Colton, R.B., and O'Brien, H.E., 2002, Geologic map of the Belt 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 450, 19 p., 2 sheets, scale 1:100,000.</edomvd>
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                <edomv>1666</edomv>
                <edomvd>Jennings, C.W., Gutierrez, C., Bryant, W., Saucedo, G., and Wills, C., 2010, Geologic Map of California: California Geological Survey Geologic Data Map GDM-2.2010</edomvd>
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            <attrdomv>
              <edom>
                <edomv>871</edomv>
                <edomvd>Love, J.D., and Christiansen, A.C., 1985, Geologic map of Wyoming: U.S. Geological Survey, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>345</edomv>
                <edomvd>Orndorff, R.C., Harrison, R.W., and Weary, D.J., 1999, Geologic map of the Eminence quadrangle, Shannon County, Missouri; United States Geological Survey, Geologic Investigations Series, USGS I-2653, scale 1:24000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>564</edomv>
                <edomvd>Orndorff, R.C., Harrison, R.W., and Weary, D.J., 1999, Geologic map of the Eminence quadrangle, Shannon County, Missouri; United States Geological Survey, Geologic Investigations Series, USGS I-2653, scale 1:24000. | Weary, D.J. and Orndorff, R.C., 2012, Geologic map of the Alley Spring Quadrangle, Shannon County, Missouri; United States Geological Survey, Scientific Investigations Map, USGS SIM-3161, scale 1:24000. | Weary, D.J., Harrison, R.W., Orndorff, R.C., Weems, R.E., Schindler, J.S., Repetski, J.E., and Pierce, H.A., 2015, Bedrock geologic map of the Spring Valley, West Plains, and parts of the Piedmont and Poplar Bluff 30' x 60' quadrangles, Missouri, including the upper Current River and Eleven Point River drainage basins; United States Geological Survey, Scientific Investigations Map, USGS SIM-3280, scale 1:100000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>520</edomv>
                <edomvd>Crane, G.W., 1906, Geologic map of the Bonne Terre 15' quadrangle, Missouri; Missouri Geological Survey, RO0601, scale 1:62500. | Crane, G.W., 1908, Geologic map of the Bonne Terre 15' quadrangle, Missouri; Missouri Geological Survey, Preliminary Map, RO0802, scale 1:62500. | Buckley, E.R., 1908, Geologic and topographic map of the Bonne Terre sheet 15' quadrangle, Missouri; Missouri Geological Survey, Volume, 2nd Series, V-009, part-2, pl-043, RO0802C, scale 1:62500.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1471</edomv>
                <edomvd>Harrison, J.E., Cressman, E.R., and Whipple, J.W., 1992, Geologic and structure maps of the Kalispell 1 x 2 degree quadrangle, Montana, and Alberta and British Columbia: U.S. Geological Survey  Miscellaneous Geologic Investigations Map 2267, 2 sheets, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1103</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1052</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1046</edomv>
                <edomvd>Scott, T.M., Campbell, K.M., Rupert, F.R., Arthur, J.D., Green, R.C., Means, G.H., Missimer, T.M., Lloyd, J.M., Yon, J.W. and Duncan, J.G., 2001, Geologic map of the state of Florida: Florida Geological Survey, Map Series 146, scale 1:1,000,000 (revised 2006).</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1491</edomv>
                <edomvd>McDonald, C., Lopez, D.A., Berg, R.B., and Gibson, R.I., 2005, Preliminary geologic map of the Ringling 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 511, 27 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>202</edomv>
                <edomvd>Pratt, W.P., Middendorf, M.A., Satterfield, I.R., and Gerdemann, P.E., 1992, Geologic map of the Rolla 1° X 2° quadrangle, Missouri [color]; United States Geological Survey, Miscellaneous Investigations Series Map, USGS I-1998, scale 1:250000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1044</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1463</edomv>
                <edomvd>O'Neill, J.M., and Christiansen, R.L., 2002, Geologic map of the Hebgen Lake 30' x 60' quadrangle, Beaverhead, Madison, and Gallatin counties, Montana, Park and Teton counties, Wyoming, and Clark and Fremont Counties, Idaho: Montana Bureau of Mines and Geology Open-File Report 464, 21 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>562</edomv>
                <edomvd>Orndorff, R.C., Harrison, R.W., and Weary, D.J., 1999, Geologic map of the Eminence quadrangle, Shannon County, Missouri; United States Geological Survey, Geologic Investigations Series, USGS I-2653, scale 1:24000. | McDowell, R.C. and Harrison, R.W., 2000, Geologic map of the Powder Mill Ferry quadrangle, Shannon and Reynolds counties, Missouri; United States Geological Survey, Geologic Investigations Series, USGS I-2722, scale 1:24000. | Orndorff, R.C. and Harrison, R.W., 2001, Geologic map of the Winona quadrangle, Shannon County, Missouri; United States Geological Survey, Geologic Investigations Series, USGS I-2749, scale 1:24000. | Weary, D.J., Harrison, R.W., Orndorff, R.C., Weems, R.E., Schindler, J.S., Repetski, J.E., and Pierce, H.A., 2015, Bedrock geologic map of the Spring Valley, West Plains, and parts of the Piedmont and Poplar Bluff 30' x 60' quadrangles, Missouri, including the upper Current River and Eleven Point River drainage basins; United States Geological Survey, Scientific Investigations Map, USGS SIM-3280, scale 1:100000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1011</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>881</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1638</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>409</edomv>
                <edomvd>Harrison, R.W., Orndorff, R.C., and Weary, D.J., 2002, Geologic map of the Stegall Mountain 7.5-minute quadrangle, Shannon and Carter counties, Missouri; United States Geological Survey, Geologic Investigations Series, USGS I-2767, scale 1:24000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1073</edomv>
                <edomvd>Noger, M.C., 1988, Geologic map of Kentucky: U.S. Geological Survey, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>528</edomv>
                <edomvd>Pratt, W.P., Middendorf, M.A., Satterfield, I.R., and Gerdemann, P.E., 1992, Geologic map of the Rolla 1° X 2° quadrangle, Missouri [color]; United States Geological Survey, Miscellaneous Investigations Series Map, USGS I-1998, scale 1:250000. | Stewart, D.R. and Aid, Kenneth, 1951, Geologic map of the Fredericktown 15' quadrangle, Missouri; Missouri Geological Survey, RO5106, scale 1:48000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>788</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>623</edomv>
                <edomvd>Slucher, E.R., Swinford, E.M., Larsen, G.E., Schumacher, G.A., Shrake, D.L., Rice, C.L., Caudill, M.R., Rea, R.G., and Powers, D.M., 2006, Bedrock geologic map of Ohio: Ohio Division of Geological Survey, Map BG-1, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>907</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1029</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>614</edomv>
                <edomvd>Rickard, L.V., Isachsen, Y.W., and Fisher, D.W., 1970, Geologic Map of New York: New York State Museum and Science Service Map and Chart Series 15 (Explanatory sheet published in 1971), 5 sheets, scale 1:250,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>941</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>999</edomv>
                <edomvd>Sims, P.K., 1992, Geologic map of Precambrian rocks, southern Lake Superior region, Wisconsin and northern Michigan: U.S. Geological Survey Miscellaneous Investigations Series Map I-2185, scale: 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>666</edomv>
                <edomvd>Ratcliffe, N.M., Stanley, R.S., Gale, M.H., Thompson, P.J., Walsh, G.J., Hatch, N.L., Rankin, D.W., Doolan, B.L., Kim, Jonathan, Mehrtens, C.J., Aleinikoff, J.N., McHone, J.G., and Masonic, L.M., 2011, Bedrock Geologic Map of Vermont: U.S. Geological Survey Scientific Investigations Map SIM-3184, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>936</edomv>
                <edomvd>This Report</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1443</edomv>
                <edomvd>Ruppel, E.T., O'Neill, J.M., and Lopez, D.A., 1993, Geologic map of the Dillon 1 x 2 degree quadrangle, Montana and Idaho: U.S. Geological Survey Miscellaneous Geologic Investigations Map 1803-H, 1 sheet, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1453</edomv>
                <edomvd>Berg, R.B., Lonn, J.D., and Locke, W.W., 1999, Geologic map of the Gardiner 30' x 60' quadrangle, south-central Montana: Montana Bureau of Mines and Geology Open-File Report 387, 11 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1522</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1496</edomv>
                <edomvd>Lewis, R.S., Burmester, R.F., Breckenridge, R.M., McFaddan, M.D., and Phillips, W.M., 2008, Preliminary geologic map of the Sandpoint 30' x 60' quadrangle, Idaho and Montana, and the Idaho part of the Chewelah 30' x 60' quadrangle: Idaho Geological Survey, Digital Web Map DWM-94, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>664</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1639</edomv>
                <edomvd>U.S. Geological Survey, 2014, USGS Small-scale Dataset - 1:1,000,000-Scale Coastline of the United States 201403 Shapefile: U.S. Geological Survey Data Release, https://www.sciencebase.gov/catalog/item/581d051de4b08da350d523be.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1500</edomv>
                <edomvd>Mudge, M.R., Earhart, R.L., Whipple, J.W., and Harrison, J.E., 1983, Geologic and structure maps of the Choteau 1 x 2 degree quadrangle, northwestern Montana: Montana Bureau of Mines and Geology Montana Atlas 3-A, 2 sheets, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>347</edomv>
                <edomvd>Brown, V.M., 1983, Geology [of exposed Precambrian rocks] of the Des Arc NE 7 1/2' quadrangle, southeast Missouri; Missouri Geological Survey, Open-File Map, OFM-84-198-GI, scale 1:24000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>530</edomv>
                <edomvd>Walker, T.H., 1942, Bedrock geologic map of the northwest quarter of the Ironton 15' quadrangle, Missouri; Missouri Geological Survey, RO4205, scale 1:48000. | Berry, A.W., Jr., 1970, Geologic map of a portion of the Taum Sauk Caldera, St. Francois Mountains, Missouri; Missouri Geological Survey, RO7001, scale 1:24000. | McCracken, Mary H., 1971, Structural features of Missouri; Missouri Geological Survey and Water Resources, RI-049, vi+99 p., 1 pl., 11 figs.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>843</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>816</edomv>
                <edomvd>Jirsa, M.A., Boerboom, T.J., and Chandler, V.W., 2012, Geologic Map of Minnesota, Precambrian bedrock geology: Minnesota Geological Survey State Map Series S-22, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1479</edomv>
                <edomvd>Lonn, J.D., McDonald, C., Sears, J.W., and Smith, L.N., 2010, Geologic map of the Missoula East 30' x 60' quadrangle, western Montana: Montana Bureau of Mines and Geology Open-File Report 593, 2 sheets, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>337</edomv>
                <edomvd>Robertson, F.S., 1961, Precambrian geology of the St. Francois Mountains in the Ironton 15' quadrangle, Missouri; Missouri Geological Survey, RO6101, scale 1:62500. | Marko, P.J., 1964, Geologic map of the Knoblick area, St. Francois County, Missouri; Missouri Geological Survey, RO6401, scale 1:31700.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1095</edomv>
                <edomvd>Martin, J.E., Sawyer, J.F., Fahrenbach, M.D., Tomhave, D.W., and Schulz, L.D., 2004, Geologic map of South Dakota: South Dakota Geological Survey General Map G-10, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>908</edomv>
                <edomvd>Virginia Division of Mineral Resources, 1993, Geologic map of Virginia, Virginia Division of Mineral Resources, series unknown, 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>848</edomv>
                <edomvd>North Carolina Geological Survey, 1985, Geologic map of North Carolina: North Carolina Geological Survey General Geologic Map, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>225</edomv>
                <edomvd>Berry, A.W., Jr., 1976, Geologic map of the western portion of the Taum Sauk caldera, St. Francois Mountains, Missouri; Missouri Geological Survey, Report of Investigations, RI-061, RO7603, scale 1:90000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1442</edomv>
                <edomvd>Vuke, S.M., 2014, Preliminary geologic map of the Dearborn River 30' x 60' quadrangle, west-central Montana: Montana Bureau of Mines and Geology Open-File Report 649, 9 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1444</edomv>
                <edomvd>Bergantino, R.N., 2001, Geologic map of the Dodson 30' x 60' quadrangle, north-central Montana: Montana Bureau of Mines and Geology Open-File Report 439, 9 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1424</edomv>
                <edomvd>Porter, K.W., Wilde, E.M., and Vuke, S.M., 1996, Preliminary geologic map of the Big Snowy Mountains 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 341, 16 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1517</edomv>
                <edomvd>Porter, K.W., and Wilde, E.M., 2001, Geologic map of the Zortman 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 438, 16 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>940</edomv>
                <edomvd>Witzke, B.J., Anderson, R.R., and Pope, J.P., 2010, Bedrock Geologic Map of Iowa: Iowa Geological Survey Open-File Map OFM-2010-01, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>334</edomv>
                <edomvd>Robertson, F.S., 1961, Precambrian geology of the St. Francois Mountains in the Ironton 15' quadrangle, Missouri; Missouri Geological Survey, RO6101, scale 1:62500.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1656</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>783</edomv>
                <edomvd>Sims, P.K., Bankey, V., Finn, C.A., 2001, Preliminary Precambrian basement map of Colorado-a geologic interpretation of the aeromagnetic anomaly map: U.S. Geological Survey Open-File Report 01-364, scale 1:1,000,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>655</edomv>
                <edomvd>Tomhave, D.W., and Schulz, L.D., 2004, Bedrock geologic map showing configuration of the bedrock surface in South Dakota east of the Missouri River: South Dakota Geological Survey General Map 9, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>932</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>606</edomv>
                <edomvd>Tiger US State 2021 (tl_2021_us_state.SHP)</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1472</edomv>
                <edomvd>Lonn, J.D., Skipp, B., Ruppel, E.T., Janecke, S.U., Perry Jr., W.J., Sears, J.W., Bartholomew, M.J., Stickney, M.C., Fritz, W.J., Hurlow, H.A., and Thomas, R.C., 2000, Geologic map of the Lima 30' x 60' quadrangle, southwest Montana: Montana Bureau of Mines and Geology Open-File Report 408, 42 p., 2 sheets, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1035</edomv>
                <edomvd>Tweto, Ogden, 1979, Geologic map of Colorado: U.S. Geological Survey, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>371</edomv>
                <edomvd>Nusbaum, R.L., 1978, [Bedrock geologic map of the Iron Mountain Lake 7.5' quadrangle, Missouri]; Missouri Geological Survey, RO7813B, scale 1:24000.</edomvd>
                <edomvds>This report</edomvds>
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            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1435</edomv>
                <edomvd>Reynolds, M.W., and Brandt, T.R., 2005, Geologic map of the Canyon Ferry Dam 30' x 60' quadrangle, west-central Montana: U.S. Geological Survey Scientific Investigations Map 2860, 32 p., 3 sheets, scale 1:100,000. .</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1498</edomv>
                <edomvd>Mudge, M.R., Earhart, R.L., Whipple, J.W., and Harrison, J.E., 1983, Geologic and structure maps of the Choteau 1 x 2 degree quadrangle, northwestern Montana: Montana Bureau of Mines and Geology Montana Atlas 3-A, 2 sheets, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>339</edomv>
                <edomvd>Marko, P.J., 1964, Geologic map of the Knoblick area, St. Francois County, Missouri; Missouri Geological Survey, RO6401, scale 1:31700. | Stewart, D.R. and Aid, Kenneth, 1943, Preliminary geologic map of the Fredericktown district, Missouri; Missouri Geological Survey, Manuscript file, MSC-1535, RO4301, scale 1:62500.</edomvd>
                <edomvds>This report</edomvds>
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            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>596</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>368</edomv>
                <edomvd>Robertson, F.S., 1961, Precambrian geology of the St. Francois Mountains in the Ironton 15' quadrangle, Missouri; Missouri Geological Survey, RO6101, scale 1:62500. | Amos, D.H. and Desborough, G.A., 1970, Geologic map of parts of the Ironton and Fredericktown areas, Missouri; Missouri Geological Survey, Report of Investigations, RI-047, pl-1, RO7003, scale 1:36000. | Pratt, W.P., Middendorf, M.A., Satterfield, I.R., and Gerdemann, P.E., 1992, Geologic map of the Rolla 1° X 2° quadrangle, Missouri [color]; United States Geological Survey, Miscellaneous Investigations Series Map, USGS I-1998, scale 1:250000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1507</edomv>
                <edomvd>Lonn, J.D., and McFaddan, M.D., 1999, Geologic map of the Montana part of the Wallace 30' x 60' quadrangle: Montana Bureau of Mines and Geology Open-File Report 388, 15 p., 2 sheets, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>649</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1065</edomv>
                <edomvd>Kansas Geological Survey, 2008, Surficial Geology of Kansas: Kansas Geological Survey, Map M-118, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>2</edomv>
                <edomvd>Starbuck, E.A., 2017, Geologic map of Missouri, 2017; Missouri Geological Survey, GM-02-2017, scale 1:500000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>338</edomv>
                <edomvd>Marko, P.J., 1964, Geologic map of the Knoblick area, St. Francois County, Missouri; Missouri Geological Survey, RO6401, scale 1:31700.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>877</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>794</edomv>
                <edomvd>Anderson, R., 2006, Geology of the Precambrian surface of Iowa and surrounding area: Iowa Geological Survey Open File Map OFM-06-7, scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>342</edomv>
                <edomvd>Lemmon, R.D., 1964, Areal geologic map of the Slabtown Granite in the Fredericktown 15' quadrangle, Missouri; Missouri Geological Survey, RO6403, scale 1:43700.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1494</edomv>
                <edomvd>Lonn,J.D., Elliott, C.G., Lewis, R.S., Burmester, R.F., McFaddan, M.D., Stanford, L.R., and Jänecke, S.U., 2019, Geologic map of the Montana part of the Salmon 30' x 60' quadrangle, southwestern Montana: Montana Bureau of Mines and Geology Geologic Map 75, 28 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1005</edomv>
                <edomvd>U.S. Geological Survey, 2014, USGS Small-scale Dataset - 1:1,000,000-Scale Coastline of the United States 201403 Shapefile: U.S. Geological Survey Data Release, https://www.sciencebase.gov/catalog/item/581d051de4b08da350d523be.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>527</edomv>
                <edomvd>Pratt, W.P., Middendorf, M.A., Satterfield, I.R., and Gerdemann, P.E., 1992, Geologic map of the Rolla 1° X 2° quadrangle, Missouri [color]; United States Geological Survey, Miscellaneous Investigations Series Map, USGS I-1998, scale 1:250000. | Satterfield, I.R., 1980, Reconnaissance geologic map of the Higdon 7 1/2' quadrangle, Missouri; Missouri Geological Survey, RO8003, scale 1:24000. | Satterfield, I.R., 1980, Reconnaissance geologic map of the Hurricane 7 1/2' quadrangle, Missouri; Missouri Geological Survey, RO8004, scale 1:24000. | Satterfield, I.R., 1981, Geologic map of the Higdon 15' quadrangle, Missouri; Missouri Geological Survey, RO8103, scale 1:62500.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1021</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>847</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>435</edomv>
                <edomvd>McDowell, R.C. and Harrison, R.W., 1998, Geologic map of the Powder Mill Ferry 7 1/2' quadrangle, Shannon and Reynolds counties, Missouri; Missouri Geological Survey, RO9803, scale 1:24000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1076</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>221</edomv>
                <edomvd>Sides, J.R., 1983, Geologic map of exposed Precambrian rocks in the Lake Killarney quadrangle, Missouri [7.5]; Missouri Geological Survey, Open-File Map, OFM-83-162-MR, scale 1:24000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>439</edomv>
                <edomvd>Weary, D.J., Harrison, R.W., Orndorff, R.C., Weems, R.E., Schindler, J.S., Repetski, J.E., and Pierce, H.A., 2015, Bedrock geologic map of the Spring Valley, West Plains, and parts of the Piedmont and Poplar Bluff 30' x 60' quadrangles, Missouri, including the upper Current River and Eleven Point River drainage basins; United States Geological Survey, Scientific Investigations Map, USGS SIM-3280, scale 1:100000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1084</edomv>
                <edomvd>Snead, J.I., and McCulloh, R.P., 1984, Geologic Map of Louisiana: Louisiana Geological Survey Geologic Map 5, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>887</edomv>
                <edomvd>Kolata, D.R., comp., 2005, Bedrock Geology of Illinois: Champaign, Ill., Illinois State Geological Survey, Illinois Map Series 14, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>952</edomv>
                <edomvd>U.S. Geological Survey, 2014, USGS Small-scale Dataset - 1:1,000,000-Scale Coastline of the United States 201403 Shapefile: U.S. Geological Survey Data Release, https://www.sciencebase.gov/catalog/item/581d051de4b08da350d523be.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>854</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1067</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1508</edomv>
                <edomvd>Reynolds, M.W., and Brandt, T.R., 2007, Preliminary geologic map of the White Sulphur Springs 30' x 60' quadrangle, Montana: U.S. Geological Survey Open-File Report 2006-1329, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>968</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1431</edomv>
                <edomvd>Lopez, D.A., 2000, Geologic map of the Bridger 30' x 60' quadrangle, Montana: Montana Bureau of Mines and Geology Geologic Map 58, 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1474</edomv>
                <edomvd>Vuke, S.M., Wilde, E.M., Lopez, D.A., and Bergantino, R.N., 2000, Geologic map of the Lodge Grass 30' x 60' quadrangle, Montana: Montana Bureau of Mines and Geology Geologic Map 56, 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>567</edomv>
                <edomvd>Harrison, R.W., Orndorff, R.C., and Weary, D.J., 2002, Geologic map of the Stegall Mountain 7.5-minute quadrangle, Shannon and Carter counties, Missouri; United States Geological Survey, Geologic Investigations Series, USGS I-2767, scale 1:24000. | Weary, D.J. and Weems, R.E., 2005, Geologic map of the Van Buren North quadrangle, Carter, Reynolds, and Shannon Counties, Missouri; United States Geological Survey, Geologic Investigations Series Map, USGS I-2802, scale 1:24000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>343</edomv>
                <edomvd>Corbitt, L.L., 1966, Geologic map of the Butler Hill Granite area in southeast Missouri; Missouri Geological Survey, RO6601, scale 1:20000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1434</edomv>
                <edomvd>McDonald, C., Elliott, C.G., Vuke, S.M., Lonn, J.D., and Berg, R.B., 2012, Geologic map of the Butte South 30' x 60' quadrangle, southwestern Montana: Montana Bureau of Mines and Geology Open-File Report 622, 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1484</edomv>
                <edomvd>Lonn, J.D., McDonald, C., Lewis, R.S., Kalakay, T.J., O'Neill, J.M., Berg, R.B., and Hargrave, P., 2003, Geologic map of the Philipsburg 30' x 60' quadrangle, western Montana: Montana Bureau of Mines and Geology Open-File Report 483, 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1485</edomv>
                <edomvd>Lonn, J.D., Smith, L.N., and McCulloch, R.B., 2007, Geologic map of the Plains 30' x 60' quadrangle, western Montana: Montana Bureau of Mines and Geology Open-File Report 554, 43 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>827</edomv>
                <edomvd>Sims, P.K., O'Neill, J.M., Bankey, V., and Anderson, E., 2004, Precambrian basement geologic map of Montana -- an interpretation of aeromagnetic anomalies: U.S. Geological Survey, Scientific Investigations Map SIM-2829, scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>197</edomv>
                <edomvd>Stewart, D.R. and Aid, Kenneth, 1951, Geologic map of the Fredericktown 15' quadrangle, Missouri; Missouri Geological Survey, RO5106, scale 1:48000. | Stewart, D.R. and Aid, Kenneth, 1943, Preliminary geologic map of the Fredericktown district, Missouri; Missouri Geological Survey, Manuscript file, MSC-1535, RO4301, scale 1:62500. | McCracken, Mary H., 1971, Structural features of Missouri; Missouri Geological Survey and Water Resources, RI-049, vi+99 p., 1 pl., 11 figs. | Satterfield, I.R., 1980, Reconnaissance geologic map of the Higdon 7 1/2' quadrangle, Missouri; Missouri Geological Survey, RO8003, scale 1:24000. | Pratt, W.P., Middendorf, M.A., Satterfield, I.R., and Gerdemann, P.E., 1992, Geologic map of the Rolla 1° X 2° quadrangle, Missouri [color]; United States Geological Survey, Miscellaneous Investigations Series Map, USGS I-1998, scale 1:250000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1464</edomv>
                <edomvd>Harrison, J.E., Whipple, J.W., and Lidke, D.J., 1998, Geologic map of the western part of the Cut Bank 1 x 2 degree quadrangle, northwestern Montana: U.S. Geological Survey Miscellaneous Geologic Investigations Map 2593, 1 sheet, scale 1:250,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>636</edomv>
                <edomvd>U.S. Geological Survey, 2014, USGS Small-scale Dataset - 1:1,000,000-Scale Coastline of the United States 201403 Shapefile: U.S. Geological Survey Data Release, https://www.sciencebase.gov/catalog/item/581d051de4b08da350d523be.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1480</edomv>
                <edomvd>Lewis, R.S., 1998, Preliminary geologic map of the Montana part of the Missoula West 30' x 60' quadrangle: Montana Bureau of Mines and Geology Open-File Report 373, 20 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>994</edomv>
                <edomvd>McCormick, K.A., 2010, Precambrian Basement Terrane of South Dakota: South Dakota Geological Survey Bulletin 41, 2 Plates, Scale 1:1,000,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>336</edomv>
                <edomvd>Anderson, R.E., 1962, Geologic map of Precambrian igneous rocks in the Taum Sauk area, Missouri; Missouri Geological Survey, RO6203, scale 1:62500. | Berry, A.W., Jr., 1976, Geologic map of the western portion of the Taum Sauk caldera, St. Francois Mountains, Missouri; Missouri Geological Survey, Report of Investigations, RI-061, RO7603, scale 1:90000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>589</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1652</edomv>
                <edomvd>Lewis, R.S., Link, P.K., Stanford, L.R., and Long, S.P., 2012, Geologic map of Idaho: Idaho Geological Survey, Map M-9, scale 1:750,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Notes</attrlabl>
            <attrdef>Additional information specific to a particular feature or table entry.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain. Free text. Values of &lt;null&gt; or #null indicate no entry.</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>ContactsAndFaults_ID</attrlabl>
            <attrdef>Primary key.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Arbitrary string. Values should be unique within this database.</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>MapSourceID</attrlabl>
            <attrdef>Identifies source map. Foreign key to DataSources table.</attrdef>
            <attrdefs>This Report</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
        </detailed>
        <detailed>
          <enttyp>
            <enttypl>MapUnitLines</enttypl>
            <enttypd>Lines that record distribution of map units of narrow, linear extent on the particular map horizon.  In the original file geodatabase, this dataset is found within the GeologicMap feature dataset.</enttypd>
            <enttypds>GeMS</enttypds>
          </enttyp>
          <attr>
            <attrlabl>OBJECTID</attrlabl>
            <attrdef>Internal feature number</attrdef>
            <attrdefs>ESRI</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Shape</attrlabl>
            <attrdef>Internal geometry object</attrdef>
            <attrdefs>ESRI</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Shape_Length</attrlabl>
            <attrdef>Internal feature length, double</attrdef>
            <attrdefs>ESRI</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>MapUnit</attrlabl>
            <attrdef>Short plain-text identifier of the map unit. Foreign key to DescriptionOfMapUnits table.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>PRu</edomv>
                <edomvd>Undifferentiated Proterozoic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>CAZms</edomv>
                <edomvd>Metasedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>PHs</edomv>
                <edomvd>Phanerozoic cover rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Zm</edomv>
                <edomvd>Metamorphic and igneous rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Zms</edomv>
                <edomvd>Metasedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>PZpCmg</edomv>
                <edomvd>Metaigneous rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Aif</edomv>
                <edomvd>Iron formation</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Xif</edomv>
                <edomvd>Iron formation</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>IsConcealed</attrlabl>
            <attrdef>Flag for contacts and faults covered by overlying map unit.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>LocationConfidenceMeters</attrlabl>
            <attrdef>Estimated half-width in meters of positional uncertainty envelope; position is relative to other features in database.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Positive real number. Value of -9, -99, or -999 indicates value is unknown.</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>ExistenceConfidence</attrlabl>
            <attrdef>Confidence that feature exists.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>certain</edomv>
                <edomvd>Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation.</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>IdentityConfidence</attrlabl>
            <attrdef>Confidence that feature is correctly identified.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>certain</edomv>
                <edomvd>Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation.</edomvd>
                <edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Label</attrlabl>
            <attrdef>Plain-text equivalent of the desired annotation for a feature: for example "14 Ma", or "^c" which (when used with the FGDC GeoAge font) results in the geologic map-unit label TRc (with TR run together to make the Triassic symbol).</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Symbol</attrlabl>
            <attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>PlotAtScale</attrlabl>
            <attrdef>At what scale (or larger) should this observation or analysis be plotted? At smaller scales, it should not be plotted. Useful to prevent crowding of display at small scales and to display progressively more data at larger and larger scales. Value is scale denominator.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Positive real number.</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>DataSourceID</attrlabl>
            <attrdef>Source of data; foreign key to table DataSources.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>816</edomv>
                <edomvd>Jirsa, M.A., Boerboom, T.J., and Chandler, V.W., 2012, Geologic Map of Minnesota, Precambrian bedrock geology: Minnesota Geological Survey State Map Series S-22, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1645</edomv>
                <edomvd>Osborne, W.E., Szabo, M.W., Copeland Jr., C.W., and Neathery, T.L., 1989, Geologic Map of Alabama: Geological Survey of Alabama Special Map 221, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1095</edomv>
                <edomvd>Martin, J.E., Sawyer, J.F., Fahrenbach, M.D., Tomhave, D.W., and Schulz, L.D., 2004, Geologic map of South Dakota: South Dakota Geological Survey General Map G-10, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1091</edomv>
                <edomvd>Thompson, D.E., 2011, Geologic Map of Mississippi; after Bickler, A.R., 1969, Geologic Map of Mississippi: Mississippi Department of Environmental Quality, Office of Geology, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>908</edomv>
                <edomvd>Virginia Division of Mineral Resources, 1993, Geologic map of Virginia, Virginia Division of Mineral Resources, series unknown, 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>623</edomv>
                <edomvd>Slucher, E.R., Swinford, E.M., Larsen, G.E., Schumacher, G.A., Shrake, D.L., Rice, C.L., Caudill, M.R., Rea, R.G., and Powers, D.M., 2006, Bedrock geologic map of Ohio: Ohio Division of Geological Survey, Map BG-1, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1073</edomv>
                <edomvd>Noger, M.C., 1988, Geologic map of Kentucky: U.S. Geological Survey, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1055</edomv>
                <edomvd>Lawton, D.E., Moye, F.J., Murray, J.B., O'Connor, B.J., Penley, H.M., Sandrock, G.S., Marsalis, W.E., Friddell, M.S., Hetrick, J.H., Huddlestun, P.F., Hunter, R.E., Mann, W.R., Martin, B.F., Pickering, S.M., Schneeberger, F.J., and Wilson, J.D., 1976, Geologic map of Georgia: Georgia Geological Survey, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>935</edomv>
                <edomvd>Gray, H.H., Ault, C.H., and Keller, S.J., 1987, Bedrock geologic map of Indiana: Indiana Geological Survey Miscellaneous Map 48, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Notes</attrlabl>
            <attrdef>Additional information specific to a particular feature or table entry.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain. Free text. Values of &lt;null&gt; or #null indicate no entry.</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>MapUnitLines_ID</attrlabl>
            <attrdef>Primary key.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <udom>Arbitrary string. Values should be unique within this database.</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>MapSourceID</attrlabl>
            <attrdef>Identifies source map. Foreign key to DataSources table.</attrdef>
            <attrdefs>This Report</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Source_MapUnit</attrlabl>
            <attrdef>Short, easily understood ASCII-character identifier for the source map unit. Prefixed with a MapSourceID value (from Source_DescriptionOfMapUnits) to differentiate identically-named source map units from different source maps. Otherwise conceptually equivalent to the "MapUnit" field in the GeMS "DescriptionOfMapUnits" table.</attrdef>
            <attrdefs>This Report</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
        </detailed>
      </eainfo>
    <distinfo>
        <distrib>
            <cntinfo>
                <cntorgp>
                    <cntorg>U.S. Geological Survey</cntorg>
                    <cntper>NGMDB</cntper>
                </cntorgp>
                <cntaddr>
                    <addrtype>mailing</addrtype>
                    <address>12201 Sunrise Valley Dr., MS 908</address>
                    <city>Reston</city>
                    <state>VA</state>
                    <postal>20192</postal>
                </cntaddr>
                <cntvoice>NA</cntvoice>
                <cntemail>ngmdb@usgs.gov</cntemail>
            </cntinfo>
        </distrib>
        <distliab>Any use of trade, product or firm names is for descriptive purposes only and does
            not
            imply endorsement by the U.S. Geological Survey. Although this information product, for
            the
            most part, is in the public domain, it also contains copyrighted materials as noted in
            the
            text. Permission to reproduce copyrighted items for other than personal use must be
            secured
            from the copyright owner. This database has been approved for release and publication by
            the
            Director of the USGS. Although this database has been subjected to rigorous review and
            is
            substantially complete, the USGS reserves the right to revise the data pursuant to
            further
            analysis and review. Furthermore, it is released on condition that neither the USGS nor
            the
            United States Government may be held liable for any damages resulting from its
            authorized or
            unauthorized use. Although these data have been processed successfully on a computer
            system at
            the U.S. Geological Survey, no warranty expressed or implied is made regarding the
            display or
            utility of the data on any other system, or for general or scientific purposes, nor
            shall the
            act of distribution constitute any such warranty. The U.S. Geological Survey shall not
            be held
            liable for improper or incorrect use of the data described and/or contained herein.</distliab>
        <stdorder>
            <digform>
                <digtinfo>
                    <formname>Digital Data</formname>
                </digtinfo>
                <digtopt>
                    <onlinopt>
                        <computer>
                          <networka>
                            <networkr>https://doi.org/10.5066/P13TSV2J</networkr>
                        </networka>
                        </computer>
                    </onlinopt>
                </digtopt>
            </digform>
            <fees>None</fees>
        </stdorder>
    </distinfo>
    <metainfo>
        <metd>20250403</metd>
        <metc>
            <cntinfo>
                <cntorgp>
                    <cntorg>U.S. Geological Survey</cntorg>
                    <cntper>NGMDB</cntper>
                </cntorgp>
                <cntaddr>
                    <addrtype>mailing</addrtype>
                    <address>12201 Sunrise Valley Dr., MS 908</address>
                    <city>Reston</city>
                    <state>VA</state>
                    <postal>20192</postal>
                </cntaddr>
                <cntvoice>NA</cntvoice>
                <cntemail>ngmdb@usgs.gov</cntemail>
            </cntinfo>
        </metc>
        <metstdn>FGDC Biological Data Profile of the Content Standard for Digital Geospatial
            Metadata</metstdn>
        <metstdv>FGDC-STD-001.1-1999</metstdv>
    </metainfo>
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