<?xml version="1.0" encoding="UTF-8"?>
<metadata>
    <idinfo>
        <citation>
            <citeinfo>
                <origin>Nolan C. Barrette, ORCID: 0000-0002-0499-6744</origin>
                <origin>Samuel A. Johnstone, ORCID: 0000-0002-3945-2499</origin>
                <origin>Juan-Marcel Campos, ORCID: 0000-0001-7811-8920</origin>
                <origin>Joseph P. Colgan, ORCID: 0000-0001-6671-1436</origin>
                <origin>Warren P. Roe, ORCID: 0000-0001-9667-1906</origin>
                <pubdate>2025</pubdate>
                <title>Cooperative National Geologic Map: Quaternary geology</title>
                <geoform>vector digital data</geoform>
                <onlink>https://doi.org/10.5066/P16SJAC6</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 Quaternary Geology layer depicts Quaternary geologic units exposed at the
                earth’s
                surface over the entire conterminous United States, inclusive of everything from
                glacial
                deposits to lava flows. This includes all units that may, or are known to, span the
                Quaternary – Neogene boundary. Where present, units older than Quaternary and map
                units that
                are primarily colluvium and/or residuum are categorized as generalized rock and
                regolith
                units. In the glaciated regions of the Midwest and Northeast, the map is a composite
                of 8
                state geologic maps depicting Quaternary deposits. In the West and parts of the
                Southeast,
                the map is a composite of Quaternary units from 19 state geologic maps depicting
                geology at
                the earth’s surface. The remaining area is populated from 18 regional Quaternary
                geologic
                maps produced as part of the USGS Quaternary Atlas series. 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_quaternary 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>1978</begdate>
                    <enddate>2023</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:d821e9ab-5eb4-4f2f-bc71-381765db0316</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>
            <attrdomv>
              <edom>
                <edomv>Qe</edomv>
                <edomvd>Eolian sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qly</edomv>
                <edomvd>Younger lacustrine sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qv</edomv>
                <edomvd>Quaternary volcanic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qel</edomv>
                <edomvd>Loess</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qes</edomv>
                <edomvd>Dune sand</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>QTcz</edomv>
                <edomvd>Coastal zone sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qpm</edomv>
                <edomvd>Peat and muck</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qls</edomv>
                <edomvd>Debris flows, landslides, and other localized mass-movement sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>QTv</edomv>
                <edomvd>Volcanic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qg</edomv>
                <edomvd>Glacial till, undifferentiated</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qczy</edomv>
                <edomvd>Younger coastal zone sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>QTm</edomv>
                <edomvd>Marine sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qm</edomv>
                <edomvd>Marine sediment</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>Qmy</edomv>
                <edomvd>Younger marine sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qay</edomv>
                <edomvd>Young alluvial sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qcz</edomv>
                <edomvd>Coastal zone sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qs</edomv>
                <edomvd>Clastic sediments, undifferentiated</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>unmapped</edomv>
                <edomvd>Unmapped area</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qai</edomv>
                <edomvd>Intermediate alluvial sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qp</edomv>
                <edomvd>Playa sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Rim</edomv>
                <edomvd>Pre-Quaternary igneous and metamorphic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qgo</edomv>
                <edomvd>Older glacial till</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Ru</edomv>
                <edomvd>Residual materials and pre-Quaternary rocks and sediments</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qico</edomv>
                <edomvd>Older ice-contact and ice-marginal sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qa</edomv>
                <edomvd>Alluvial sediment, undifferentiated</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>QTa</edomv>
                <edomvd>Alluvial sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qcsr</edomv>
                <edomvd>Quaternary chemical sedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qic</edomv>
                <edomvd>Ice-contact and ice-marginal sediment, undiferentiated</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>QTs</edomv>
                <edomvd>Sedimentary rocks, undifferentiated</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Ql</edomv>
                <edomvd>Lacustrine sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qao</edomv>
                <edomvd>Old alluvial sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </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>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>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>Other materials</edomv>
                <edomvd>Other materials</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>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>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>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>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>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>Rock and sediment</edomv>
                <edomvd>Various rocks and sediment, not differentiated.</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>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>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>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>"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>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>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>
          </attr>
          <attr>
            <attrlabl>GeoMaterialConfidence</attrlabl>
            <attrdef>Describes appropriateness of GeoMaterial term for describing the map unit.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <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>1251</edomv>
                <edomvd>Scott, T.M., Knapp, M.S., and Weide, D.L, compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., eds., 1986, Quaternary geologic map of the Florida Keys 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NG-17), scale 1:1,000,000, [Bush, C.A., Digital edition, 2010], https://pubs.usgs.gov/imap/i-1420/ng-17/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <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>
                <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>1340</edomv>
                <edomvd>Fullerton, D.S., Cowan, W.R., Savon, W.D., Goldthwait, R.P., Ferrand, W.R., Muller, E.H., Bahling, R.E., and Stravers, J.A., compilers; Fullerton, D.S., and Richmond, G.M., eds.; 1991, Quaternary Geologic Map of the Lake Erie 4° x 6° Quadrangle, United States and Canada, U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NK-17), scale 1:1,000,000, [Digital edition, 2002], https://pubs.usgs.gov/imap/i-1420/nk-17/</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>1289</edomv>
                <edomvd>Jackson, R.L, and Doctor, D.H., 2023, A geodatabase representing a compilation of Cadwell, D.H., and others, 1991, Surficial Geology of New York; New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets.: U.S. Geological Survey data release, https://doi.org/10.5066/P9KM842E</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1306</edomv>
                <edomvd>Minnesota Geologic Survey, D-01 database of Surficial Geology Of Minnesota, https://mngs-umn.opendata.arcgis.com/apps/UMN::d-01-surficial-geology-of-minnesota/about, accessed November 1st, 2023</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1257</edomv>
                <edomvd>Scott, T.M., Knapp, M.S., Friddell, M.S., and Weide, D.L, compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., eds., 1986, Quaternary geologic map of the Jacksonville 4° × 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NH-17), scale 1:1,000,000, [Bush, C.A., Digital edition, 2012], https://pubs.usgs.gov/imap/i-1420/nh-17/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <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>
              </edom>
            </attrdomv>
            <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>1293</edomv>
                <edomvd>Combination of multiple sources: Surficial Geology Material Explanation|Jackson, R.L, and Doctor, D.H., 2023, A geodatabase representing a compilation of Cadwell, D.H., and others, 1991, Surficial Geology of New York; New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets.: U.S. Geological Survey data release, https://doi.org/10.5066/P9KM842E</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>1320</edomv>
                <edomvd>Farrand, W.R., and Bell, D.L., 1982, Quaternary Geology of Northern Michigan: Michigan Department of Natural Resources, Michigan Geological Survey, Geological Publication QG-01, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1414</edomv>
                <edomvd>Farrand, W.R., and Bell, D.L., 1982, Quaternary Geology of Southern Michigan: Michigan Department of Natural Resources, Michigan Geological Survey, Geological Publication QG-01, scale 1:500,000</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>1141</edomv>
                <edomvd>Gadd, N.R., Veillete, J.J., Fullerton, D.S., Wagner, P.W., and Chapman, W.F., compilers; Fullerton, D.S., ed., 1993, Quaternary Geologic Map of the Ottawa 4° x 6° Quadrangle, United States and Canada: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NL-18), scale 1:1,000,000, [Digital edition, 2006], https://pubs.usgs.gov/imap/i-1420/nl-18/</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>1346</edomv>
                <edomvd>Borns, H.W., Gadd, N.R., LaSalle, Pierre, Martineau, Ghismond, Chauvin, Luc, Fullerton, D.S., Fulton, R.J., Chapman, W.F., Wagner, W.P., and Grant, D.R., compilers; Richmond, G.M. and Fullerton, D.S., eds., 1987, Quaternary Geologic Map of the Quebec 4°x 6° Quadrangle, United States and Canada: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NL-19), scale 1:1,000,000, [Digital edition, 2006], https://pubs.usgs.gov/imap/i-1420/nl-19/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1388</edomv>
                <edomvd>Gray, H.H., Bleuer, N.K., Lineback, J.A., Swadley, W.C., Richmond, G.M., Miller, R.A., Goldthwait, R.P., and Ward, R.A. compilers; Richmond, G.M., Fullerton, D.S., and Bush, C.A., eds., 1991, Quaternary geologic map of the Louisville 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NJ-16), scale 1:1,000,000, [Bush, C.A., Digital edition, 2011], https://pubs.usgs.gov/imap/i-1420/nj-16/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1382</edomv>
                <edomvd>Cleaves, E.T., Glaser, J.D., Howard, A.D., Johnson, G.H., Wheeler, W.H., Sevon, W.D., Sheldon, J., Owens, J.P., Peebles, P.C., compilers; Richmond, G.M., and Fullerton, D.S., Weide, D.L., eds., 1987, Quaternary geologic map of the Chesapeake Bay 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NJ-18), [Digital edition, 2006], https://pubs.usgs.gov/imap/i-1420/nj-18/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>929</edomv>
                <edomvd>Clayton, L., Moran, S.R., Bluemle, J.P., and Carlson, C.G., 1980, Geologic map of North Dakota: U.S. Geological Survey, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1669</edomv>
                <edomvd>Pavey, R. R.; Goldthwait, R. P.; Brockman, S. C., Hull, D. N., Swinford, E. M., and Van Horn, R.G, 1999, Quaternary Geology of Ohio: Ohio Division of Geological Survey, Map No. 2, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1281</edomv>
                <edomvd>Fullerton, D.S., Sevon, W.D., Muller, E.H., Judson, Sheldon, Black, R.F., Wagner, P.W., Hartshorn, J.H., Chapman, W.F., and Cowan, W.D., compilers; Fullerton, D.S., ed., 1992, Quaternary Geologic Map of the Hudson River 4° x 6° Quadrangle, United States and Canada: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NK-18), scale 1:1,000,000, [Digital edition, 2005], https://pubs.usgs.gov/imap/i-1420/nk-18/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1221</edomv>
                <edomvd>Whitfield, J.W., Ward, R.A., Denne, J.E., Holbrook, D.F., Bush, W.V., Lineback, J.A., Luza, K.V., Jensen, K.M., and Fishman, W.D., compilers, Richmond, G.M. and Weide, D.L., eds., 1994, Quaternary geologic map of the Ozark Plateau 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NJ-15), scale 1:1,000,000 [Bush, C.A., Digital edition, 2011], https://pubs.usgs.gov/imap/i-1420/nj-15/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1227</edomv>
                <edomvd>Copeland, C.W., Jr., Rheams, K.F., Neathery, T.L., Gilliland, W.A., Schmidt, Walter, Clark, W.C., Jr., and Pope, D.E., compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., eds., 1988, Quaternary geologic map of the Mobile 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NH-16), scale 1:1,000,000, [Bush, C.A., Digital edition, 2010], https://pubs.usgs.gov/imap/i-1420/nh-16/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1263</edomv>
                <edomvd>Richmond, G.M., Fullerton, D.S., and Weide, D.L., eds., Colquhoun, D.J., Friddell, M.S., Wheeler, W.H., Daniels, R.B., Gregory, J.P., Miller, R.A., and Van Nostrand, A.K., compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., eds., 1987, Quaternary geologic map of the Savannah 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NI-17), scale 1:1,000,000, [Bush, C.A., Digital edition, 2013], https://pubs.usgs.gov/imap/i-1420/ni-17/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1166</edomv>
                <edomvd>Lineback, J.A., 1979, Quaternary deposits of Illinois: Illinois State Geological Survey, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1309</edomv>
                <edomvd>Gray, H.H., 1989, Quaternary geologic map of Indiana: Indiana Geological Survey, Miscellaneous Map 49, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1134</edomv>
                <edomvd>Johnson, G.H., and Peebles, P.C., compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., and Bush, C.A., eds., 1986, Quaternary geologic map of the Hatteras 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NI-18), scale 1:1,000,000, [Bush, C.A., Digital edition, 2011], https://pubs.usgs.gov/imap/i-1420/ni-18/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1197</edomv>
                <edomvd>Holbrook, D.F., Gilliland, W.A., Luza, K.V., Pope, D.E., Wermund, E.G., Miller, R.A., Bush, W.V., Jensen, K.N., and Fishman, W.D., compilers; Richmond, G.M., Fullerton, D.S., and Weide, D.L., eds., 1990, Quaternary geologic map of the Vicksburg 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map-1420 (NI-15), scale 1:1,000,000, [Bush, C.A., Digital edition, 2012], https://pubs.usgs.gov/imap/i-1420/ni-15/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1302</edomv>
                <edomvd>Lusardi, Barbara A; Gowan, Angela S; McDonald, Jennifer M; Marshall, Katherine J; Meyer, Gary N; Wagner, Kaleb G. (2019). S-23 Geologic Map of Minnesota - Quaternary Geology. Minnesota Geological Survey. Scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1239</edomv>
                <edomvd>Farrand, W.R., Mickelson, D.M., Cowan, W.R., and Goebel, J.E., compilers; Richmond, G.M. and Fullerton, D.S., eds., 1984, Quaternary Geologic Map of the Lake Superior 4° x 6° Quadrangle, United States and Canada: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NL-16), scale 1:1,000,000, [Digital edition, 2002], https://pubs.usgs.gov/imap/i-1420/nl-16/</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>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>
                <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>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>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1316</edomv>
                <edomvd>This Report</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1128</edomv>
                <edomvd>Howard, A.D., Behling, R.E., Wheeler, W.H., Daniels, R.B., Swadley, W.C., Goldthwait, R.P., Fullerton, D.S., Sevon, W.D., Miller, R.A., compilers; Richmond, G.M., Fullerton, D.S., Christiansen, A.C., eds., 1991, Quaternary geologic map of the Blue Ridge 4° x 6° quadrangle, United States: Quaternary Geologic Atlas of the United States Map I-1420 (NJ-17), scale 1:1,000,000, [Bush, C.A., Digital edition, 2011], https://pubs.usgs.gov/imap/i-1420/nj-17/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1173</edomv>
                <edomvd>Swinehart, J.B., Dreeszen, V.H., Richmond, G.M., Tipton, M.J., Bretz, Richard, Steece, F.V., Hallberg, G.R., and Goebel, J.E., compilers; Richmond, G.M., ed., 1994, Quaternary geologic map of the Platte River 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NK-14), scale 1:1,000,000, [Digital edition, 2008], https://pubs.usgs.gov/imap/i-1420/nk-14/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1307</edomv>
                <edomvd>Combination of multiple sources: Minnesota Geologic Survey, D-01 database of Surficial Geology Of Minnesota, https://mngs-umn.opendata.arcgis.com/apps/UMN::d-01-surficial-geology-of-minnesota/about, accessed November 1st, 2023|Lusardi, Barbara A; Gowan, Angela S; McDonald, Jennifer M; Marshall, Katherine J; Meyer, Gary N; Wagner, Kaleb G. (2019). S-23 Geologic Map of Minnesota - Quaternary Geology. Minnesota Geological Survey. Scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1209</edomv>
                <edomvd>Goebel, J.E., Mickelson, D.M., Ferrand, W.R., Clayton, Lee, Knox, J.C., Cahow, Adam, Hobbs, H.C., Walton, M.S., compilers; Richmond, G.M. and Fullerton, D.S., eds., 1983, Quaternary Geologic Map of the Minneapolis 4° x 6° Quadrangle, United States: U.S. Geological Survey iscellaneous Investigations Series Map I-1420(NL-15), scale 1:1,000,000, [Digital edition, 2007], https://pubs.usgs.gov/imap/i-1420/nl-15/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1526</edomv>
                <edomvd>Digital database of the Montana state geologic map, submitted to STATEMAP in GeMS</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1376</edomv>
                <edomvd>Hartshorn, J.H., Thompson, W.B., Chapman, W.F., Black, R.F., Richmond, G.M., Grant, D.R., and Fullerton, D.S., compilers; Richmond, G.M. and Fullerton, D.S., eds., 1991, Quaternary Geologic Map of the Boston 4° x 6° Quadrangle, United States and Canada: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420(NK-19), scale 1:1,000,000, [Digital edition, 2006], https://pubs.usgs.gov/imap/i-1420/nk-19/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1191</edomv>
                <edomvd>Pope, D.E., Gilliland, W.A., and Wermund, E.G., compilers; Richmond, G.M., Weide, D.L., and Moore, D.W., eds., 1990, Quaternary geologic map of the White Lake 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NH-15), scale 1:1,000,000 [Bush, C.A., Digital edition, 2012], https://pubs.usgs.gov/imap/i-1420/nh-15/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1284</edomv>
                <edomvd>Cadwell, D.H., Dineen, R.J., Connally, G.G., Fleisher, P.J., and Rich, J.L., 1987, Surficial geologic map of New York; Hudson-Mohawk sheet: New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1031</edomv>
                <edomvd>McFarland, J.D., 1998 (revised 2004), Stratigraphic summary of Arkansas: Arkansas Geological Survey Circular 36, 38 p.</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>1185</edomv>
                <edomvd>Hallberg, G.R., Lineback, J.A., Mickelson, D.M., Knox, J.C., Goebel, J.E., Hobbs, H.C., Whitfield, J.W., Ward, R.A., Boellstorff, J.D., Swinehart, J.B., and Dreeszen, V.H., compilers; Richmond, G.M., Fullerton, D.S., and Christiansen, A.C., eds., 1994, Quaternary geologic map of the Des Moines 4° x 6° Quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NK-15), scale 1:1,000,000, [Digital edition, 2008], https://pubs.usgs.gov/imap/i-1420/nk-15/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1304</edomv>
                <edomvd>This Report</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1160</edomv>
                <edomvd>Lineback, J.A., Bleuer, N.K., Mickelson, D.M., Ferrand, W.R., and Goldthwait, R.P., compilers; Richmond, G.M., and Fullerton, D.S., eds., 1983, Quaternary geologic map of the Chicago 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NK-16), scale 1:1,000,000, [Digital edition, 2002], https://pubs.usgs.gov/imap/i-1420/nk-16/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1288</edomv>
                <edomvd>Surficial Geology Material Explanation</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>
            <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>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <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>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1400</edomv>
                <edomvd>Thompson, Woodrow B., and Borns, Harold W., Jr. (editors), 1985, Surficial geologic map of Maine: Maine Geological Survey, 42" x 52" color map, scale 1:500,000. Maine Geological Survey Maps. 15. http://digitalmaine.com/mgs_maps/15</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1115</edomv>
                <edomvd>Texas Water Science Center, 2015, Geologic database of Texas</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1233</edomv>
                <edomvd>Miller, R.A., Maher, S.W., Copeland, Jr., C.W., Rheams, K.F., Neathery, T.L., Gilliland, W.A., Friddell, M.S., Van Nostrand, A.K., Wheeler, W.H., Holbrook, D.F., and Bush, W.V., compilers; Richmond, G.M., and Fullerton, D.S., eds., 1988, Quaternary geologic map of the Lookout Mountain 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NI-16), scale 1:1,000,000 [Bush, C.A., Digital edition, 2013], https://pubs.usgs.gov/imap/i-1420/ni-16/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <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>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1411</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>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>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>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>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>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>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>Rock</edomv>
                <edomvd>Various rock types, not differentiated.</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>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>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>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>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Source_DescriptionOfMapUnits_ID</attrlabl>
            <attrdef>Primary key on the Source_DescriptionOfMapUnits table.</attrdef>
            <attrdefs>This Report</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
        </detailed>
        <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>
            <attrlabl>OBJECTID</attrlabl>
            <attrdef>Internal feature number</attrdef>
            <attrdefs>ESRI</attrdefs>
            <attrdomv>
              <udom>Unrepresentable domain</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_DescriptionOfMapUnitsID</attrlabl>
            <attrdef>Foreign key to DescriptionOfMapUnits 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>
          <attr>
            <attrlabl>DescriptionOfMapUnitsID</attrlabl>
            <attrdef>Foreign key to DescriptionOfMapUnits table.</attrdef>
            <attrdefs>This Report</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>Qe</edomv>
                <edomvd>Eolian sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qly</edomv>
                <edomvd>Younger lacustrine sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qv</edomv>
                <edomvd>Quaternary volcanic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qel</edomv>
                <edomvd>Loess</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qes</edomv>
                <edomvd>Dune sand</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>QTcz</edomv>
                <edomvd>Coastal zone sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qpm</edomv>
                <edomvd>Peat and muck</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qls</edomv>
                <edomvd>Debris flows, landslides, and other localized mass-movement sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>QTv</edomv>
                <edomvd>Volcanic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qg</edomv>
                <edomvd>Glacial till, undifferentiated</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qczy</edomv>
                <edomvd>Younger coastal zone sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>QTm</edomv>
                <edomvd>Marine sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qm</edomv>
                <edomvd>Marine sediment</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>Qmy</edomv>
                <edomvd>Younger marine sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qay</edomv>
                <edomvd>Young alluvial sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qcz</edomv>
                <edomvd>Coastal zone sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qs</edomv>
                <edomvd>Clastic sediments, undifferentiated</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>unmapped</edomv>
                <edomvd>Unmapped area</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qai</edomv>
                <edomvd>Intermediate alluvial sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qp</edomv>
                <edomvd>Playa sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Rim</edomv>
                <edomvd>Pre-Quaternary igneous and metamorphic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qgo</edomv>
                <edomvd>Older glacial till</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Ru</edomv>
                <edomvd>Residual materials and pre-Quaternary rocks and sediments</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qico</edomv>
                <edomvd>Older ice-contact and ice-marginal sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qa</edomv>
                <edomvd>Alluvial sediment, undifferentiated</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qic</edomv>
                <edomvd>Ice-contact and ice-marginal sediment, undiferentiated</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qcsr</edomv>
                <edomvd>Quaternary chemical sedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>QTa</edomv>
                <edomvd>Alluvial sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>QTs</edomv>
                <edomvd>Sedimentary rocks, undifferentiated</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Ql</edomv>
                <edomvd>Lacustrine sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qao</edomv>
                <edomvd>Old alluvial sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
          </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>
            <attrdomv>
              <udom>Unrepresentable domain</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Symbol_Lookup_ID</attrlabl>
            <attrdef>Primary key on the Symbol_Lookup table.</attrdef>
            <attrdefs>This Report</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>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>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>shoreline scarp</edomv>
                <edomvd>A line of cliffs with lateral continuity produced by erosion along a shoreline.</edomvd>
                <edomvds>This Report</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>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>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>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>beach ridges</edomv>
                <edomvd>A low, essentially continuous mound of beach or beach-and-dune material (sand, gravel, shingle) on the backshore of a beach beyond the present limit of storm waves or the reach of ordinary tides, and occurring singly or as one of a series of approximately parallel deposits. The ridges are roughly parallel to the shoreline and represent successive positions of an advancing shoreline. Called "cheniers" in southern Louisiana, for the oak trees that often grow on them.</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>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>limit of significant glacial advance</edomv>
                <edomvd>The extent reached by the glacier during an interval of positive net balance. Often corresponds with significant sediment deposition.</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>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>
            <attrdomv>
              <edom>
                <edomv>outcrop</edomv>
                <edomvd>That part of a geologic formation or structure that appears at the surface of the Earth.</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>
          </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>
          </attr>
        </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>Qe</edomv>
                <edomvd>Eolian sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qly</edomv>
                <edomvd>Younger lacustrine sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qv</edomv>
                <edomvd>Quaternary volcanic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qel</edomv>
                <edomvd>Loess</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>QTcz</edomv>
                <edomvd>Coastal zone sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qes</edomv>
                <edomvd>Dune sand</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qls</edomv>
                <edomvd>Debris flows, landslides, and other localized mass-movement sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qpm</edomv>
                <edomvd>Peat and muck</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>QTv</edomv>
                <edomvd>Volcanic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qg</edomv>
                <edomvd>Glacial till, undifferentiated</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qczy</edomv>
                <edomvd>Younger coastal zone sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>QTm</edomv>
                <edomvd>Marine sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qm</edomv>
                <edomvd>Marine sediment</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>Qmy</edomv>
                <edomvd>Younger marine sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qay</edomv>
                <edomvd>Young alluvial sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qcz</edomv>
                <edomvd>Coastal zone sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qs</edomv>
                <edomvd>Clastic sediments, undifferentiated</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>unmapped</edomv>
                <edomvd>Unmapped area</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qai</edomv>
                <edomvd>Intermediate alluvial sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qp</edomv>
                <edomvd>Playa sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Rim</edomv>
                <edomvd>Pre-Quaternary igneous and metamorphic rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qgo</edomv>
                <edomvd>Older glacial till</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Ru</edomv>
                <edomvd>Residual materials and pre-Quaternary rocks and sediments</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qico</edomv>
                <edomvd>Older ice-contact and ice-marginal sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qa</edomv>
                <edomvd>Alluvial sediment, undifferentiated</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qic</edomv>
                <edomvd>Ice-contact and ice-marginal sediment, undiferentiated</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qcsr</edomv>
                <edomvd>Quaternary chemical sedimentary rocks</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>QTa</edomv>
                <edomvd>Alluvial sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>QTs</edomv>
                <edomvd>Sedimentary rocks, undifferentiated</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Ql</edomv>
                <edomvd>Lacustrine sediment</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>Qao</edomv>
                <edomvd>Old alluvial sediment</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>1251</edomv>
                <edomvd>Scott, T.M., Knapp, M.S., and Weide, D.L, compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., eds., 1986, Quaternary geologic map of the Florida Keys 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NG-17), scale 1:1,000,000, [Bush, C.A., Digital edition, 2010], https://pubs.usgs.gov/imap/i-1420/ng-17/</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>1340</edomv>
                <edomvd>Fullerton, D.S., Cowan, W.R., Savon, W.D., Goldthwait, R.P., Ferrand, W.R., Muller, E.H., Bahling, R.E., and Stravers, J.A., compilers; Fullerton, D.S., and Richmond, G.M., eds.; 1991, Quaternary Geologic Map of the Lake Erie 4° x 6° Quadrangle, United States and Canada, U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NK-17), scale 1:1,000,000, [Digital edition, 2002], https://pubs.usgs.gov/imap/i-1420/nk-17/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1624</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>1542</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>1595</edomv>
                <edomvd>Vuke, S.M., Heffern, E.L., Bergantino, R.N., and Colton, R.B., 2001, Geologic map of the Powderville 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 429, 8 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1613</edomv>
                <edomvd>Berg, R.B., 2002, Geologic map of the Valier 30' x 60' quadrangle, northwestern Montana: Montana Bureau of Mines and Geology Open-File Report 453, 10 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1582</edomv>
                <edomvd>Lopez, D.A., 2002, Geologic map of the Lonesome Lake 30' x 60' quadrangle, north-central Montana: Montana Bureau of Mines and Geology Open-File Report 446, 13 p., 1 sheet, scale 1:100,000.</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>1619</edomv>
                <edomvd>Wilde, E.M., and Porter, K.W., 2002, Geologic map of the Winifred 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 437, 13 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1589</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>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1530</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>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1414</edomv>
                <edomvd>Farrand, W.R., and Bell, D.L., 1982, Quaternary Geology of Southern Michigan: Michigan Department of Natural Resources, Michigan Geological Survey, Geological Publication QG-01, scale 1:500,000</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>1614</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>929</edomv>
                <edomvd>Clayton, L., Moran, S.R., Bluemle, J.P., and Carlson, C.G., 1980, Geologic map of North Dakota: U.S. Geological Survey, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1563</edomv>
                <edomvd>Vuke, S.M., Colton, R.B., and Fullerton, D.S., 2002, Geologic map of the Great Falls North 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 459, 13 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1227</edomv>
                <edomvd>Copeland, C.W., Jr., Rheams, K.F., Neathery, T.L., Gilliland, W.A., Schmidt, Walter, Clark, W.C., Jr., and Pope, D.E., compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., eds., 1988, Quaternary geologic map of the Mobile 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NH-16), scale 1:1,000,000, [Bush, C.A., Digital edition, 2010], https://pubs.usgs.gov/imap/i-1420/nh-16/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1626</edomv>
                <edomvd>Vuke, S.M., Porter, K.W., Lonn, J.D., and Lopez, D.A., 2007, Geologic map of Montana [Earth surface version]: Montana Bureau of Mines and Geology Geologic Map 62, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1309</edomv>
                <edomvd>Gray, H.H., 1989, Quaternary geologic map of Indiana: Indiana Geological Survey, Miscellaneous Map 49, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1574</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>1560</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>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>1587</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>1566</edomv>
                <edomvd>Vuke, S.M., Wilde, E.M., and Bergantino, R.N., 2000, Geologic map of the Hardin 30' x 60' quadrangle, Montana: Montana Bureau of Mines and Geology Geologic Map 57, 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1583</edomv>
                <edomvd>Bergantino, R.N., 1999, Geologic and structure contour maps of the Malta 30' x 60' quadrangle, northeastern Montana: Montana Bureau of Mines and Geology Open-File Report 389, 4 p., 2 sheets, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1592</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>1597</edomv>
                <edomvd>Wilde, E.M., and Smith, L.N., 2003, Geologic and structure contour map of the Richey 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 475, 9 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1564</edomv>
                <edomvd>Vuke, S.M., 2000, Geologic map of the Great Falls South 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 407, 18 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1545</edomv>
                <edomvd>Vuke, S.M., Hargrave, P.A., and Smith, L.N., 2011, Geologic map of the Circle 30' x 60' quadrangle Dawson, McCone, and Prairie counties, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 597, 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1569</edomv>
                <edomvd>Sholes, M.A., and Bergantino, R.N., 2002, Geologic map of the Havre 30' x 60' quadrangle, north-central Montana: Montana Bureau of Mines and Geology Open-File Report 467, 8 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1575</edomv>
                <edomvd>Vuke, S.M., Heffern, E.L., Bergantino, R.N., and Colton, R.B., 2001, Geologic map of the Lame Deer 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 428, 8 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1536</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>1608</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>1286</edomv>
                <edomvd>Muller, E.H., Cadwell, D.H., Connally, G.G., Young, R.A., 1986, Surficial geologic map of New York; Finger Lakes sheet: New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>1558</edomv>
                <edomvd>Wilde, E.M., and Bergantino, R.N., 2004, Geologic and structure contour map of the Fort Peck Lake East 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 498, 10 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1577</edomv>
                <edomvd>Porter, K.W., and Wilde, E.M., 1993, Geologic map of the Lewistown 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 308, 22 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1561</edomv>
                <edomvd>Bergantino, R.N., 1999, Geologic map of the Glasgow 30' x 60' quadrangle, northeast Montana: Montana Bureau of Mines and Geology Open-File Report 390, 4 p., 2 sheets, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1296</edomv>
                <edomvd>Combination of multiple sources: Cadwell, D.H., Dineen, R.J., Connally, G.G., Fleisher, P.J., and Rich, J.L., 1987, Surficial geologic map of New York; Hudson-Mohawk sheet: New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets|Jackson, R.L, and Doctor, D.H., 2023, A geodatabase representing a compilation of Cadwell, D.H., and others, 1991, Surficial Geology of New York; New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets.: U.S. Geological Survey data release, https://doi.org/10.5066/P9KM842E</edomvd>
                <edomvds>This report</edomvds>
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              <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>
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                <edomv>1611</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>
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              <edom>
                <edomv>1287</edomv>
                <edomvd>Cadwell, D.H., Connally, G.G., Fleisher, P.J., Muller, E.H., 1988, Surficial geologic map of New York; Niagara sheet: New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>1591</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>
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              <edom>
                <edomv>1233</edomv>
                <edomvd>Miller, R.A., Maher, S.W., Copeland, Jr., C.W., Rheams, K.F., Neathery, T.L., Gilliland, W.A., Friddell, M.S., Van Nostrand, A.K., Wheeler, W.H., Holbrook, D.F., and Bush, W.V., compilers; Richmond, G.M., and Fullerton, D.S., eds., 1988, Quaternary geologic map of the Lookout Mountain 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NI-16), scale 1:1,000,000 [Bush, C.A., Digital edition, 2013], https://pubs.usgs.gov/imap/i-1420/ni-16/</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1605</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>
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              <edom>
                <edomv>1411</edomv>
                <edomvd>This Report</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>1590</edomv>
                <edomvd>Bergantino, R.N., 2001, Geologic and structure contour map of the Opheim 30' x 60' quadrangle, northeast Montana: Montana Bureau of Mines and Geology Open-File Report 440, 6 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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                <edomv>1618</edomv>
                <edomvd>Vuke, S.M., Wilde, E.M., Colton, R.B., and Stickney, M.C., 2003, Geologic map of the Wibaux 30' x 60' quadrangle, eastern Montana and adjacent North Dakota: Montana Bureau of Mines and Geology Open-File Report 465, 11 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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                <edomv>1544</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>
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                <edomv>1601</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>
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              <edom>
                <edomv>1306</edomv>
                <edomvd>Minnesota Geologic Survey, D-01 database of Surficial Geology Of Minnesota, https://mngs-umn.opendata.arcgis.com/apps/UMN::d-01-surficial-geology-of-minnesota/about, accessed November 1st, 2023</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1594</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>
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              <edom>
                <edomv>1531</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>
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            <attrdomv>
              <edom>
                <edomv>1621</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>1620</edomv>
                <edomvd>Porter, K.W., and Wilde, E.M., 1993, Geologic map of the Winnett 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 307, 16 p., 2 sheets, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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                <edomv>1283</edomv>
                <edomvd>Cadwell, D.H., Connally, G.G., Dineen, R.J., Fleisher, P.J., Fuller, M.L., Les Sirkin, M.L., and Wiles, G.C., 1989, Surficial geologic map of New York; Lower Hudson sheet: New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1572</edomv>
                <edomvd>Vuke, S.M., Wilde, E.M., and Bergantino, R.N., 2003, Geologic map of the Hysham 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 486, 10 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1141</edomv>
                <edomvd>Gadd, N.R., Veillete, J.J., Fullerton, D.S., Wagner, P.W., and Chapman, W.F., compilers; Fullerton, D.S., ed., 1993, Quaternary Geologic Map of the Ottawa 4° x 6° Quadrangle, United States and Canada: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NL-18), scale 1:1,000,000, [Digital edition, 2006], https://pubs.usgs.gov/imap/i-1420/nl-18/</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1346</edomv>
                <edomvd>Borns, H.W., Gadd, N.R., LaSalle, Pierre, Martineau, Ghismond, Chauvin, Luc, Fullerton, D.S., Fulton, R.J., Chapman, W.F., Wagner, W.P., and Grant, D.R., compilers; Richmond, G.M. and Fullerton, D.S., eds., 1987, Quaternary Geologic Map of the Quebec 4°x 6° Quadrangle, United States and Canada: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NL-19), scale 1:1,000,000, [Digital edition, 2006], https://pubs.usgs.gov/imap/i-1420/nl-19/</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1609</edomv>
                <edomvd>Lopez, D.A., 2002, Geologic map of the Sweet Grass Hills 30' x 60' quadrangle, north-central Montana: Montana Bureau of Mines and Geology Open-File Report 443, 18 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
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                <edomvd>Gray, H.H., Bleuer, N.K., Lineback, J.A., Swadley, W.C., Richmond, G.M., Miller, R.A., Goldthwait, R.P., and Ward, R.A. compilers; Richmond, G.M., Fullerton, D.S., and Bush, C.A., eds., 1991, Quaternary geologic map of the Louisville 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NJ-16), scale 1:1,000,000, [Bush, C.A., Digital edition, 2011], https://pubs.usgs.gov/imap/i-1420/nj-16/</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1382</edomv>
                <edomvd>Cleaves, E.T., Glaser, J.D., Howard, A.D., Johnson, G.H., Wheeler, W.H., Sevon, W.D., Sheldon, J., Owens, J.P., Peebles, P.C., compilers; Richmond, G.M., and Fullerton, D.S., Weide, D.L., eds., 1987, Quaternary geologic map of the Chesapeake Bay 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NJ-18), [Digital edition, 2006], https://pubs.usgs.gov/imap/i-1420/nj-18/</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>1600</edomv>
                <edomvd>Wilde, E.M., and Porter, K.W., 2000, Geologic map of the Roundup 30' X 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 404, 14 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
              <edom>
                <edomv>1617</edomv>
                <edomvd>Bergantino, R.N., 2003, Geologic and structure contour map of the Whitewater 30' x 60' quadrangle, northeastern Montana: Montana Bureau of Mines and Geology Open-File Report 471, 6 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>1604</edomv>
                <edomvd>Bergantino, R.N., and Wilde, E.M., 1998, Preliminary geologic and structure contour map of the Scobey 30' x 60' quadrangle, northeastern Montana: Montana Bureau of Mines and Geology Open-File Report 360, 5 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1221</edomv>
                <edomvd>Whitfield, J.W., Ward, R.A., Denne, J.E., Holbrook, D.F., Bush, W.V., Lineback, J.A., Luza, K.V., Jensen, K.M., and Fishman, W.D., compilers, Richmond, G.M. and Weide, D.L., eds., 1994, Quaternary geologic map of the Ozark Plateau 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NJ-15), scale 1:1,000,000 [Bush, C.A., Digital edition, 2011], https://pubs.usgs.gov/imap/i-1420/nj-15/</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1616</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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                <edomv>1603</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>
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                <edomv>1166</edomv>
                <edomvd>Lineback, J.A., 1979, Quaternary deposits of Illinois: Illinois State Geological Survey, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1134</edomv>
                <edomvd>Johnson, G.H., and Peebles, P.C., compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., and Bush, C.A., eds., 1986, Quaternary geologic map of the Hatteras 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NI-18), scale 1:1,000,000, [Bush, C.A., Digital edition, 2011], https://pubs.usgs.gov/imap/i-1420/ni-18/</edomvd>
                <edomvds>This report</edomvds>
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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>
                <edomvds>This report</edomvds>
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                <edomv>1573</edomv>
                <edomvd>Wilde, E.M., and Vuke, S.M., 2004, Geologic map of the Jordan 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 514, 8 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
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            <attrdomv>
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                <edomv>1576</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>
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            <attrdomv>
              <edom>
                <edomv>1570</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>
              <edom>
                <edomv>1550</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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                <edomvd>Howard, A.D., Behling, R.E., Wheeler, W.H., Daniels, R.B., Swadley, W.C., Goldthwait, R.P., Fullerton, D.S., Sevon, W.D., Miller, R.A., compilers; Richmond, G.M., Fullerton, D.S., Christiansen, A.C., eds., 1991, Quaternary geologic map of the Blue Ridge 4° x 6° quadrangle, United States: Quaternary Geologic Atlas of the United States Map I-1420 (NJ-17), scale 1:1,000,000, [Bush, C.A., Digital edition, 2011], https://pubs.usgs.gov/imap/i-1420/nj-17/</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1578</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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                <edomv>1534</edomv>
                <edomvd>Lopez, D.A., 2000, Geologic map of the Billings 30' x 60' quadrangle, Montana: Montana Bureau of Mines and Geology Geologic Map 59, 1 sheet, scale 1:100,000.</edomvd>
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                <edomv>1571</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>
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                <edomvd>Hallberg, G.R., Lineback, J.A., Mickelson, D.M., Knox, J.C., Goebel, J.E., Hobbs, H.C., Whitfield, J.W., Ward, R.A., Boellstorff, J.D., Swinehart, J.B., and Dreeszen, V.H., compilers; Richmond, G.M., Fullerton, D.S., and Christiansen, A.C., eds., 1994, Quaternary geologic map of the Des Moines 4° x 6° Quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NK-15), scale 1:1,000,000, [Digital edition, 2008], https://pubs.usgs.gov/imap/i-1420/nk-15/</edomvd>
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                <edomv>1602</edomv>
                <edomvd>Wilde, E.M., and Vuke. S.M., 2004, Geologic map of the Sand Springs 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 515, 8 p., 1 sheet, scale 1:100,000.</edomvd>
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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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                <edomv>1599</edomv>
                <edomvd>Bergantino, R.N., Porter, K.W., and Hearn Jr., B.C., 2002, Geologic map of the Rocky Boy 30' x 60' quadrangle, north-central Montana: Montana Bureau of Mines and Geology Open-File Report 451, 16 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1585</edomv>
                <edomvd>Vuke, S.M., Luft, S.J., Colton, R.B., and Heffern, E.L., 2001, Geologic map of the Miles City 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 426, 11 p., 1 sheet, scale 1:100,000.</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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                <edomv>1553</edomv>
                <edomvd>Vuke, S.M., Wilde, E.M., Bergantino, R.N., and Colton, R.B., 2001, Geologic map of the Ekalaka 30' x 60' quadrangle, eastern Montana and adjacent North and South Dakota: Montana Bureau of Mines and Geology Open-File Report 430, 11 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1581</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>
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                <edomv>1562</edomv>
                <edomvd>Vuke, S.M., and Colton R.B., 1998, Geologic map of the Glendive 30' x 60' quadrangle, eastern Montana and adjacent North Dakota: Montana Bureau of Mines and Geology Open-File Report 371, 8 p., scale 1:100,000.</edomvd>
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                <edomv>1543</edomv>
                <edomvd>Lopez, D.A., 2002, Geologic map of the Chester 30' x 60' quadrangle, north-central Montana: Montana Bureau of Mines and Geology Open-File Report 445, 11 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1598</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>
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                <edomv>1533</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>
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                <edomv>1540</edomv>
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                <edomv>1557</edomv>
                <edomvd>Berg, R.B., and Vuke, S.M., 2002, Geologic map of the Fort Benton 30' x 60' quadrangle, north-central Montana: Montana Bureau of Mines and Geology Open-File Report 460, 13 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
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                <edomvd>Combination of multiple sources: Muller, E.H., Cadwell, D.H., Connally, G.G., Young, R.A., 1986, Surficial geologic map of New York; Finger Lakes sheet: New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets|Jackson, R.L, and Doctor, D.H., 2023, A geodatabase representing a compilation of Cadwell, D.H., and others, 1991, Surficial Geology of New York; New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets.: U.S. Geological Survey data release, https://doi.org/10.5066/P9KM842E</edomvd>
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                <edomv>1567</edomv>
                <edomvd>Bergantino, R.N., Patton, T.W., and Sholes, M.A., 2003, Geologic and structure contour map of the Harlem 30' x 60' quadrangle, north-central Montana: Montana Bureau of Mines and Geology Open-File Report 468, 7 p., 1 sheet, scale 1:100,000.</edomvd>
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                <edomv>1548</edomv>
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                <edomv>1615</edomv>
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                <edomv>1547</edomv>
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                <edomv>1612</edomv>
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                <edomv>1607</edomv>
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                <edomv>1596</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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                <edomv>1549</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>
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                <edomv>1537</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>
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                <edomv>1554</edomv>
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                <edomv>1527</edomv>
                <edomvd>Vuke, S.M., Wilde, E.M., Colton, R.B., and Bergantino, R.N., 2001, Geologic map of the Alzada 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 433, 9 p., 1 sheet, scale 1:100,000.</edomvd>
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                <edomvd>This Report</edomvd>
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                <edomvd>Swinehart, J.B., Dreeszen, V.H., Richmond, G.M., Tipton, M.J., Bretz, Richard, Steece, F.V., Hallberg, G.R., and Goebel, J.E., compilers; Richmond, G.M., ed., 1994, Quaternary geologic map of the Platte River 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NK-14), scale 1:1,000,000, [Digital edition, 2008], https://pubs.usgs.gov/imap/i-1420/nk-14/</edomvd>
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                <edomvd>Digital database of the Montana state geologic map, submitted to STATEMAP in GeMS</edomvd>
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                <edomvd>Cadwell, D.H., Dineen, R.J., Connally, G.G., Fleisher, P.J., and Rich, J.L., 1987, Surficial geologic map of New York; Hudson-Mohawk sheet: New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets</edomvd>
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                <edomv>1555</edomv>
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                <edomv>1588</edomv>
                <edomvd>Porter, K.W., and Wilde, E.M, 1999, Geologic map of the Musselshell 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 386, 22 p., 1 sheet, scale 1:100,000.</edomvd>
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                <edomv>1285</edomv>
                <edomvd>Cadwell, D.H., et al., 1991, Surficial geologic map of New York; Adirondack sheet: New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets</edomvd>
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                <edomv>1551</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>
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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>
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                <edomvd>Thompson, Woodrow B., and Borns, Harold W., Jr. (editors), 1985, Surficial geologic map of Maine: Maine Geological Survey, 42" x 52" color map, scale 1:500,000. Maine Geological Survey Maps. 15. http://digitalmaine.com/mgs_maps/15</edomvd>
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                <edomv>1209</edomv>
                <edomvd>Goebel, J.E., Mickelson, D.M., Ferrand, W.R., Clayton, Lee, Knox, J.C., Cahow, Adam, Hobbs, H.C., Walton, M.S., compilers; Richmond, G.M. and Fullerton, D.S., eds., 1983, Quaternary Geologic Map of the Minneapolis 4° x 6° Quadrangle, United States: U.S. Geological Survey iscellaneous Investigations Series Map I-1420(NL-15), scale 1:1,000,000, [Digital edition, 2007], https://pubs.usgs.gov/imap/i-1420/nl-15/</edomvd>
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                <edomv>1257</edomv>
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                <edomv>1528</edomv>
                <edomvd>Vuke, S.M., Wilde, E.M., and Bergantino, R.N., 2003, Geologic map of the Angela 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 485, 10 p., 1 sheet, scale 1:100,000.</edomvd>
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                <edomv>1580</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>
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                <edomv>1586</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>
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                <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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                <edomv>1529</edomv>
                <edomvd>Vuke, S.M., Wilde, E.M., Colton, R.B., and Stickney, M.C., 2001, Geologic map of the Baker 30' x 60' quadrangle, eastern Montana and adjacent North Dakota: Montana Bureau of Mines and Geology Open-File Report 427, 9 p., 1 sheet, scale 1:100,000.</edomvd>
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                <edomv>1556</edomv>
                <edomvd>Vuke, S.M., Bergantino, R.N., Colton, R.B., Wilde, E.M., and Heffern, E.L., 2001, Geologic map of the Forsyth 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 425, 11 p., 1 sheet, scale 1:100,000.</edomvd>
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                <edomvd>This Report</edomvd>
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                <edomv>1532</edomv>
                <edomvd>Lopez, D.A., 2000, Geologic map of the Big Timber 30' x 60' quadrangle, south-central Montana: Montana Bureau of Mines and Geology Open-File Report 405, 17 p., 1 sheet, scale 1:100,000.</edomvd>
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                <edomv>1320</edomv>
                <edomvd>Farrand, W.R., and Bell, D.L., 1982, Quaternary Geology of Northern Michigan: Michigan Department of Natural Resources, Michigan Geological Survey, Geological Publication QG-01, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1297</edomv>
                <edomvd>Combination of multiple sources: Cadwell, D.H., et al., 1991, Surficial geologic map of New York; Adirondack sheet: New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets|Jackson, R.L, and Doctor, D.H., 2023, A geodatabase representing a compilation of Cadwell, D.H., and others, 1991, Surficial Geology of New York; New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets.: U.S. Geological Survey data release, https://doi.org/10.5066/P9KM842E</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>1610</edomv>
                <edomvd>Vuke, S.M., and Colton, R.B., 2003, Geologic map of the Terry 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 477, 9 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1281</edomv>
                <edomvd>Fullerton, D.S., Sevon, W.D., Muller, E.H., Judson, Sheldon, Black, R.F., Wagner, P.W., Hartshorn, J.H., Chapman, W.F., and Cowan, W.D., compilers; Fullerton, D.S., ed., 1992, Quaternary Geologic Map of the Hudson River 4° x 6° Quadrangle, United States and Canada: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NK-18), scale 1:1,000,000, [Digital edition, 2005], https://pubs.usgs.gov/imap/i-1420/nk-18/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1669</edomv>
                <edomvd>Pavey, R. R.; Goldthwait, R. P.; Brockman, S. C., Hull, D. N., Swinford, E. M., and Van Horn, R.G, 1999, Quaternary Geology of Ohio: Ohio Division of Geological Survey, Map No. 2, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1539</edomv>
                <edomvd>Vuke, S.M., Heffern, E.L., Bergantino, R.N., and Colton, R.B., 2001, Geologic map of the Broadus 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 432, 13 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1197</edomv>
                <edomvd>Holbrook, D.F., Gilliland, W.A., Luza, K.V., Pope, D.E., Wermund, E.G., Miller, R.A., Bush, W.V., Jensen, K.N., and Fishman, W.D., compilers; Richmond, G.M., Fullerton, D.S., and Weide, D.L., eds., 1990, Quaternary geologic map of the Vicksburg 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map-1420 (NI-15), scale 1:1,000,000, [Bush, C.A., Digital edition, 2012], https://pubs.usgs.gov/imap/i-1420/ni-15/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1239</edomv>
                <edomvd>Farrand, W.R., Mickelson, D.M., Cowan, W.R., and Goebel, J.E., compilers; Richmond, G.M. and Fullerton, D.S., eds., 1984, Quaternary Geologic Map of the Lake Superior 4° x 6° Quadrangle, United States and Canada: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NL-16), scale 1:1,000,000, [Digital edition, 2002], https://pubs.usgs.gov/imap/i-1420/nl-16/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1565</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>1584</edomv>
                <edomvd>Vuke, S.M., and Wilde, E.M., 2004, Geologic map of the Melstone 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 513, 12 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>1559</edomv>
                <edomvd>Wilde, E.M., and Bergantino, R.N., 2004, Geologic and structure contour map of the Fort Peck Lake West 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 499, 8 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1579</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>1541</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>1606</edomv>
                <edomvd>Vuke, S.M., Wilde, E.M., and Smith, L.N., 2003, Geologic and structure contour map of the Sidney 30' x 60' quadrangle, eastern Montana and adjacent North Dakota: Montana Bureau of Mines and Geology Open-File Report 478, 10 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1623</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>1568</edomv>
                <edomvd>Wilde, E.M., and Porter, K.W., 2001, Geologic map of the Harlowton 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 434, 20 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1538</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>1622</edomv>
                <edomvd>Bergantino, R.N., and Wilde, E.M., 1998, Preliminary geologic map of the Wolf Point 30' x 60' quadrangle: Montana Bureau of Mines and Geology Open-File Report 358, 5 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1535</edomv>
                <edomvd>Vuke, S.M., Heffern, E.L., Bergantino, R.N., and Colton, R.B., 2001, Geologic map of the Birney 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 431, 12 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1263</edomv>
                <edomvd>Richmond, G.M., Fullerton, D.S., and Weide, D.L., eds., Colquhoun, D.J., Friddell, M.S., Wheeler, W.H., Daniels, R.B., Gregory, J.P., Miller, R.A., and Van Nostrand, A.K., compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., eds., 1987, Quaternary geologic map of the Savannah 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NI-17), scale 1:1,000,000, [Bush, C.A., Digital edition, 2013], https://pubs.usgs.gov/imap/i-1420/ni-17/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1593</edomv>
                <edomvd>Bergantino, R.N., and Wilde, E.M., 1998, Preliminary geologic map of the Plentywood 30' x 60' quadrangle, northeast Montana: Montana Bureau of Mines and Geology Open-File Report 361, 5 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1294</edomv>
                <edomvd>Combination of multiple sources: Cadwell, D.H., Connally, G.G., Dineen, R.J., Fleisher, P.J., Fuller, M.L., Les Sirkin, M.L., and Wiles, G.C., 1989, Surficial geologic map of New York; Lower Hudson sheet: New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets|Jackson, R.L, and Doctor, D.H., 2023, A geodatabase representing a compilation of Cadwell, D.H., and others, 1991, Surficial Geology of New York; New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets.: U.S. Geological Survey data release, https://doi.org/10.5066/P9KM842E</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>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>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>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>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>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>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>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>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>
            <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>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>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>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>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>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>
          </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>1251</edomv>
                <edomvd>Scott, T.M., Knapp, M.S., and Weide, D.L, compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., eds., 1986, Quaternary geologic map of the Florida Keys 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NG-17), scale 1:1,000,000, [Bush, C.A., Digital edition, 2010], https://pubs.usgs.gov/imap/i-1420/ng-17/</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>1340</edomv>
                <edomvd>Fullerton, D.S., Cowan, W.R., Savon, W.D., Goldthwait, R.P., Ferrand, W.R., Muller, E.H., Bahling, R.E., and Stravers, J.A., compilers; Fullerton, D.S., and Richmond, G.M., eds.; 1991, Quaternary Geologic Map of the Lake Erie 4° x 6° Quadrangle, United States and Canada, U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NK-17), scale 1:1,000,000, [Digital edition, 2002], https://pubs.usgs.gov/imap/i-1420/nk-17/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1624</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>1542</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>1595</edomv>
                <edomvd>Vuke, S.M., Heffern, E.L., Bergantino, R.N., and Colton, R.B., 2001, Geologic map of the Powderville 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 429, 8 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1613</edomv>
                <edomvd>Berg, R.B., 2002, Geologic map of the Valier 30' x 60' quadrangle, northwestern Montana: Montana Bureau of Mines and Geology Open-File Report 453, 10 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1582</edomv>
                <edomvd>Lopez, D.A., 2002, Geologic map of the Lonesome Lake 30' x 60' quadrangle, north-central Montana: Montana Bureau of Mines and Geology Open-File Report 446, 13 p., 1 sheet, scale 1:100,000.</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>1619</edomv>
                <edomvd>Wilde, E.M., and Porter, K.W., 2002, Geologic map of the Winifred 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 437, 13 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1589</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>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1530</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>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1414</edomv>
                <edomvd>Farrand, W.R., and Bell, D.L., 1982, Quaternary Geology of Southern Michigan: Michigan Department of Natural Resources, Michigan Geological Survey, Geological Publication QG-01, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1311</edomv>
                <edomvd>US Census State Borders</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>1614</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>929</edomv>
                <edomvd>Clayton, L., Moran, S.R., Bluemle, J.P., and Carlson, C.G., 1980, Geologic map of North Dakota: U.S. Geological Survey, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1417</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>1563</edomv>
                <edomvd>Vuke, S.M., Colton, R.B., and Fullerton, D.S., 2002, Geologic map of the Great Falls North 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 459, 13 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>1227</edomv>
                <edomvd>Copeland, C.W., Jr., Rheams, K.F., Neathery, T.L., Gilliland, W.A., Schmidt, Walter, Clark, W.C., Jr., and Pope, D.E., compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., eds., 1988, Quaternary geologic map of the Mobile 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NH-16), scale 1:1,000,000, [Bush, C.A., Digital edition, 2010], https://pubs.usgs.gov/imap/i-1420/nh-16/</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>1036</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1626</edomv>
                <edomvd>Vuke, S.M., Porter, K.W., Lonn, J.D., and Lopez, D.A., 2007, Geologic map of Montana [Earth surface version]: Montana Bureau of Mines and Geology Geologic Map 62, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1309</edomv>
                <edomvd>Gray, H.H., 1989, Quaternary geologic map of Indiana: Indiana Geological Survey, Miscellaneous Map 49, scale 1:500,000</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>1574</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>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>1560</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>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>1566</edomv>
                <edomvd>Vuke, S.M., Wilde, E.M., and Bergantino, R.N., 2000, Geologic map of the Hardin 30' x 60' quadrangle, Montana: Montana Bureau of Mines and Geology Geologic Map 57, 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1587</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>1583</edomv>
                <edomvd>Bergantino, R.N., 1999, Geologic and structure contour maps of the Malta 30' x 60' quadrangle, northeastern Montana: Montana Bureau of Mines and Geology Open-File Report 389, 4 p., 2 sheets, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1592</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>1597</edomv>
                <edomvd>Wilde, E.M., and Smith, L.N., 2003, Geologic and structure contour map of the Richey 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 475, 9 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1545</edomv>
                <edomvd>Vuke, S.M., Hargrave, P.A., and Smith, L.N., 2011, Geologic map of the Circle 30' x 60' quadrangle Dawson, McCone, and Prairie counties, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 597, 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1564</edomv>
                <edomvd>Vuke, S.M., 2000, Geologic map of the Great Falls South 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 407, 18 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1569</edomv>
                <edomvd>Sholes, M.A., and Bergantino, R.N., 2002, Geologic map of the Havre 30' x 60' quadrangle, north-central Montana: Montana Bureau of Mines and Geology Open-File Report 467, 8 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1575</edomv>
                <edomvd>Vuke, S.M., Heffern, E.L., Bergantino, R.N., and Colton, R.B., 2001, Geologic map of the Lame Deer 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 428, 8 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1536</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>1608</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>1286</edomv>
                <edomvd>Muller, E.H., Cadwell, D.H., Connally, G.G., Young, R.A., 1986, Surficial geologic map of New York; Finger Lakes sheet: New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1558</edomv>
                <edomvd>Wilde, E.M., and Bergantino, R.N., 2004, Geologic and structure contour map of the Fort Peck Lake East 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 498, 10 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1577</edomv>
                <edomvd>Porter, K.W., and Wilde, E.M., 1993, Geologic map of the Lewistown 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 308, 22 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1561</edomv>
                <edomvd>Bergantino, R.N., 1999, Geologic map of the Glasgow 30' x 60' quadrangle, northeast Montana: Montana Bureau of Mines and Geology Open-File Report 390, 4 p., 2 sheets, scale 1:100,000.</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>1611</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>1287</edomv>
                <edomvd>Cadwell, D.H., Connally, G.G., Fleisher, P.J., Muller, E.H., 1988, Surficial geologic map of New York; Niagara sheet: New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1591</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>1233</edomv>
                <edomvd>Miller, R.A., Maher, S.W., Copeland, Jr., C.W., Rheams, K.F., Neathery, T.L., Gilliland, W.A., Friddell, M.S., Van Nostrand, A.K., Wheeler, W.H., Holbrook, D.F., and Bush, W.V., compilers; Richmond, G.M., and Fullerton, D.S., eds., 1988, Quaternary geologic map of the Lookout Mountain 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NI-16), scale 1:1,000,000 [Bush, C.A., Digital edition, 2013], https://pubs.usgs.gov/imap/i-1420/ni-16/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1605</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>611</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1590</edomv>
                <edomvd>Bergantino, R.N., 2001, Geologic and structure contour map of the Opheim 30' x 60' quadrangle, northeast Montana: Montana Bureau of Mines and Geology Open-File Report 440, 6 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1618</edomv>
                <edomvd>Vuke, S.M., Wilde, E.M., Colton, R.B., and Stickney, M.C., 2003, Geologic map of the Wibaux 30' x 60' quadrangle, eastern Montana and adjacent North Dakota: Montana Bureau of Mines and Geology Open-File Report 465, 11 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1303</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1544</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>645</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1601</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>1306</edomv>
                <edomvd>Minnesota Geologic Survey, D-01 database of Surficial Geology Of Minnesota, https://mngs-umn.opendata.arcgis.com/apps/UMN::d-01-surficial-geology-of-minnesota/about, accessed November 1st, 2023</edomvd>
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                <edomv>1548</edomv>
                <edomvd>Berg, R.B., 2002, Geologic map of the Cut Bank 30' x 60' quadrangle, northwestern Montana: Montana Bureau of Mines and Geology Open-File Report 454, 10 p., 1 sheet, scale 1:100,000.</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>1615</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>1044</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1547</edomv>
                <edomvd>Bergantino, R.N., and Wilde, E.M., 1998, Preliminary geologic map of the Culbertson 30' x 60' quadrangle, northeastern Montana and northwestern North Dakota: Montana Bureau of Mines and Geology Open-File Report 359, 5 p., 1 sheet, scale 1:100,000.</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>1546</edomv>
                <edomvd>Lopez, D.A., 2002, Geologic map of the Conrad 30' x 60' quadrangle, north-central Montana: Montana Bureau of Mines and Geology Open-File Report 444, 11 p., 1 sheet, scale 1:100,000.</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>
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            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1612</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>1607</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>1596</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>
                <edomvds>This report</edomvds>
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            </attrdomv>
            <attrdomv>
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                <edomv>1549</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>1527</edomv>
                <edomvd>Vuke, S.M., Wilde, E.M., Colton, R.B., and Bergantino, R.N., 2001, Geologic map of the Alzada 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 433, 9 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1537</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>
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                <edomv>1554</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>
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            </attrdomv>
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              <edom>
                <edomv>664</edomv>
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                <edomvds>This report</edomvds>
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                <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>
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                <edomv>1173</edomv>
                <edomvd>Swinehart, J.B., Dreeszen, V.H., Richmond, G.M., Tipton, M.J., Bretz, Richard, Steece, F.V., Hallberg, G.R., and Goebel, J.E., compilers; Richmond, G.M., ed., 1994, Quaternary geologic map of the Platte River 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NK-14), scale 1:1,000,000, [Digital edition, 2008], https://pubs.usgs.gov/imap/i-1420/nk-14/</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>843</edomv>
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                <edomvds>This report</edomvds>
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                <edomv>1526</edomv>
                <edomvd>Digital database of the Montana state geologic map, submitted to STATEMAP in GeMS</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1376</edomv>
                <edomvd>Hartshorn, J.H., Thompson, W.B., Chapman, W.F., Black, R.F., Richmond, G.M., Grant, D.R., and Fullerton, D.S., compilers; Richmond, G.M. and Fullerton, D.S., eds., 1991, Quaternary Geologic Map of the Boston 4° x 6° Quadrangle, United States and Canada: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420(NK-19), scale 1:1,000,000, [Digital edition, 2006], https://pubs.usgs.gov/imap/i-1420/nk-19/</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1552</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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                <edomv>1284</edomv>
                <edomvd>Cadwell, D.H., Dineen, R.J., Connally, G.G., Fleisher, P.J., and Rich, J.L., 1987, Surficial geologic map of New York; Hudson-Mohawk sheet: New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets</edomvd>
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                <edomv>1555</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>
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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>1588</edomv>
                <edomvd>Porter, K.W., and Wilde, E.M, 1999, Geologic map of the Musselshell 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 386, 22 p., 1 sheet, scale 1:100,000.</edomvd>
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              </edom>
            </attrdomv>
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                <edomvds>This report</edomvds>
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                <edomv>1285</edomv>
                <edomvd>Cadwell, D.H., et al., 1991, Surficial geologic map of New York; Adirondack sheet: New York State Museum Map and Chart Series 40, scale 1:250,000, 5 sheets</edomvd>
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                <edomv>1551</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>
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              </edom>
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                <edomv>1400</edomv>
                <edomvd>Thompson, Woodrow B., and Borns, Harold W., Jr. (editors), 1985, Surficial geologic map of Maine: Maine Geological Survey, 42" x 52" color map, scale 1:500,000. Maine Geological Survey Maps. 15. http://digitalmaine.com/mgs_maps/15</edomvd>
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                <edomv>1209</edomv>
                <edomvd>Goebel, J.E., Mickelson, D.M., Ferrand, W.R., Clayton, Lee, Knox, J.C., Cahow, Adam, Hobbs, H.C., Walton, M.S., compilers; Richmond, G.M. and Fullerton, D.S., eds., 1983, Quaternary Geologic Map of the Minneapolis 4° x 6° Quadrangle, United States: U.S. Geological Survey iscellaneous Investigations Series Map I-1420(NL-15), scale 1:1,000,000, [Digital edition, 2007], https://pubs.usgs.gov/imap/i-1420/nl-15/</edomvd>
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                <edomv>1528</edomv>
                <edomvd>Vuke, S.M., Wilde, E.M., and Bergantino, R.N., 2003, Geologic map of the Angela 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 485, 10 p., 1 sheet, scale 1:100,000.</edomvd>
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                <edomvd>Scott, T.M., Knapp, M.S., Friddell, M.S., and Weide, D.L, compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., eds., 1986, Quaternary geologic map of the Jacksonville 4° × 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NH-17), scale 1:1,000,000, [Bush, C.A., Digital edition, 2012], https://pubs.usgs.gov/imap/i-1420/nh-17/</edomvd>
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                <edomvds>This report</edomvds>
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                <edomv>1580</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>
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                <edomvds>This report</edomvds>
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                <edomv>1586</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>
            <attrdomv>
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                <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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                <edomv>1401</edomv>
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                <edomvds>This report</edomvds>
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                <edomv>1529</edomv>
                <edomvd>Vuke, S.M., Wilde, E.M., Colton, R.B., and Stickney, M.C., 2001, Geologic map of the Baker 30' x 60' quadrangle, eastern Montana and adjacent North Dakota: Montana Bureau of Mines and Geology Open-File Report 427, 9 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1556</edomv>
                <edomvd>Vuke, S.M., Bergantino, R.N., Colton, R.B., Wilde, E.M., and Heffern, E.L., 2001, Geologic map of the Forsyth 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 425, 11 p., 1 sheet, scale 1:100,000.</edomvd>
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                <edomvds>This report</edomvds>
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                <edomvds>This report</edomvds>
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                <edomv>1532</edomv>
                <edomvd>Lopez, D.A., 2000, Geologic map of the Big Timber 30' x 60' quadrangle, south-central Montana: Montana Bureau of Mines and Geology Open-File Report 405, 17 p., 1 sheet, scale 1:100,000.</edomvd>
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                <edomv>1320</edomv>
                <edomvd>Farrand, W.R., and Bell, D.L., 1982, Quaternary Geology of Northern Michigan: Michigan Department of Natural Resources, Michigan Geological Survey, Geological Publication QG-01, scale 1:500,000</edomvd>
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                <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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                <edomv>649</edomv>
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                <edomvds>This report</edomvds>
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                <edomv>869</edomv>
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                <edomvds>This report</edomvds>
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                <edomv>1610</edomv>
                <edomvd>Vuke, S.M., and Colton, R.B., 2003, Geologic map of the Terry 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 477, 9 p., 1 sheet, scale 1:100,000.</edomvd>
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                <edomvd>Pavey, R. R.; Goldthwait, R. P.; Brockman, S. C., Hull, D. N., Swinford, E. M., and Van Horn, R.G, 1999, Quaternary Geology of Ohio: Ohio Division of Geological Survey, Map No. 2, scale 1:500,000</edomvd>
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                <edomv>1021</edomv>
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                <edomvds>This report</edomvds>
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                <edomvds>This report</edomvds>
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                <edomv>1539</edomv>
                <edomvd>Vuke, S.M., Heffern, E.L., Bergantino, R.N., and Colton, R.B., 2001, Geologic map of the Broadus 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 432, 13 p., 1 sheet, scale 1:100,000.</edomvd>
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                <edomvds>This report</edomvds>
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                <edomv>1239</edomv>
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            <attrdomv>
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                <edomv>1584</edomv>
                <edomvd>Vuke, S.M., and Wilde, E.M., 2004, Geologic map of the Melstone 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 513, 12 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
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                <edomv>1565</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>
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            <attrdomv>
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                <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>
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                <edomv>1559</edomv>
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                <edomv>1579</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>854</edomv>
                <edomvd>US Census State Borders</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1541</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>1606</edomv>
                <edomvd>Vuke, S.M., Wilde, E.M., and Smith, L.N., 2003, Geologic and structure contour map of the Sidney 30' x 60' quadrangle, eastern Montana and adjacent North Dakota: Montana Bureau of Mines and Geology Open-File Report 478, 10 p., 1 sheet, scale 1:100,000.</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>1538</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>1568</edomv>
                <edomvd>Wilde, E.M., and Porter, K.W., 2001, Geologic map of the Harlowton 30' x 60' quadrangle, central Montana: Montana Bureau of Mines and Geology Open-File Report 434, 20 p., 1 sheet, 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>1622</edomv>
                <edomvd>Bergantino, R.N., and Wilde, E.M., 1998, Preliminary geologic map of the Wolf Point 30' x 60' quadrangle: Montana Bureau of Mines and Geology Open-File Report 358, 5 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1623</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>1535</edomv>
                <edomvd>Vuke, S.M., Heffern, E.L., Bergantino, R.N., and Colton, R.B., 2001, Geologic map of the Birney 30' x 60' quadrangle, eastern Montana: Montana Bureau of Mines and Geology Open-File Report 431, 12 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1673</edomv>
                <edomvd>US Census State Borders</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>1263</edomv>
                <edomvd>Richmond, G.M., Fullerton, D.S., and Weide, D.L., eds., Colquhoun, D.J., Friddell, M.S., Wheeler, W.H., Daniels, R.B., Gregory, J.P., Miller, R.A., and Van Nostrand, A.K., compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., eds., 1987, Quaternary geologic map of the Savannah 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NI-17), scale 1:1,000,000, [Bush, C.A., Digital edition, 2013], https://pubs.usgs.gov/imap/i-1420/ni-17/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1593</edomv>
                <edomvd>Bergantino, R.N., and Wilde, E.M., 1998, Preliminary geologic map of the Plentywood 30' x 60' quadrangle, northeast Montana: Montana Bureau of Mines and Geology Open-File Report 361, 5 p., 1 sheet, scale 1:100,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1415</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>GeologicLines</enttypl>
            <enttypd>Lines that represent dikes, coal seams, ash beds, fold hinge-surface traces, isograds, and other linear features. All have these properties: (A) They do not participate in map-unit topology. (B) They correspond to features that exist within the Earth and may be concealed beneath younger, covering, material. (C) They are located with an accuracy that likely can be estimated. 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>beach ridges</edomv>
                <edomvd>A low, essentially continuous mound of beach or beach-and-dune material (sand, gravel, shingle) on the backshore of a beach beyond the present limit of storm waves or the reach of ordinary tides, and occurring singly or as one of a series of approximately parallel deposits. The ridges are roughly parallel to the shoreline and represent successive positions of an advancing shoreline. Called "cheniers" in southern Louisiana, for the oak trees that often grow on them.</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 scarp</edomv>
                <edomvd>A line of cliffs with lateral continuity produced by erosion along a shoreline.</edomvd>
                <edomvds>This Report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>limit of significant glacial advance</edomv>
                <edomvd>The extent reached by the glacier during an interval of positive net balance. Often corresponds with significant sediment deposition.</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>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>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>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>DataSourceID</attrlabl>
            <attrdef>Source of data; foreign key to table DataSources.</attrdef>
            <attrdefs>GeMS</attrdefs>
            <attrdomv>
              <edom>
                <edomv>1251</edomv>
                <edomvd>Scott, T.M., Knapp, M.S., and Weide, D.L, compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., eds., 1986, Quaternary geologic map of the Florida Keys 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NG-17), scale 1:1,000,000, [Bush, C.A., Digital edition, 2010], https://pubs.usgs.gov/imap/i-1420/ng-17/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1340</edomv>
                <edomvd>Fullerton, D.S., Cowan, W.R., Savon, W.D., Goldthwait, R.P., Ferrand, W.R., Muller, E.H., Bahling, R.E., and Stravers, J.A., compilers; Fullerton, D.S., and Richmond, G.M., eds.; 1991, Quaternary Geologic Map of the Lake Erie 4° x 6° Quadrangle, United States and Canada, U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NK-17), scale 1:1,000,000, [Digital edition, 2002], https://pubs.usgs.gov/imap/i-1420/nk-17/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1257</edomv>
                <edomvd>Scott, T.M., Knapp, M.S., Friddell, M.S., and Weide, D.L, compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., eds., 1986, Quaternary geologic map of the Jacksonville 4° × 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NH-17), scale 1:1,000,000, [Bush, C.A., Digital edition, 2012], https://pubs.usgs.gov/imap/i-1420/nh-17/</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>
            <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>1388</edomv>
                <edomvd>Gray, H.H., Bleuer, N.K., Lineback, J.A., Swadley, W.C., Richmond, G.M., Miller, R.A., Goldthwait, R.P., and Ward, R.A. compilers; Richmond, G.M., Fullerton, D.S., and Bush, C.A., eds., 1991, Quaternary geologic map of the Louisville 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NJ-16), scale 1:1,000,000, [Bush, C.A., Digital edition, 2011], https://pubs.usgs.gov/imap/i-1420/nj-16/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1382</edomv>
                <edomvd>Cleaves, E.T., Glaser, J.D., Howard, A.D., Johnson, G.H., Wheeler, W.H., Sevon, W.D., Sheldon, J., Owens, J.P., Peebles, P.C., compilers; Richmond, G.M., and Fullerton, D.S., Weide, D.L., eds., 1987, Quaternary geologic map of the Chesapeake Bay 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NJ-18), [Digital edition, 2006], https://pubs.usgs.gov/imap/i-1420/nj-18/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>929</edomv>
                <edomvd>Clayton, L., Moran, S.R., Bluemle, J.P., and Carlson, C.G., 1980, Geologic map of North Dakota: U.S. Geological Survey, scale 1:500,000</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>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1281</edomv>
                <edomvd>Fullerton, D.S., Sevon, W.D., Muller, E.H., Judson, Sheldon, Black, R.F., Wagner, P.W., Hartshorn, J.H., Chapman, W.F., and Cowan, W.D., compilers; Fullerton, D.S., ed., 1992, Quaternary Geologic Map of the Hudson River 4° x 6° Quadrangle, United States and Canada: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NK-18), scale 1:1,000,000, [Digital edition, 2005], https://pubs.usgs.gov/imap/i-1420/nk-18/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1669</edomv>
                <edomvd>Pavey, R. R.; Goldthwait, R. P.; Brockman, S. C., Hull, D. N., Swinford, E. M., and Van Horn, R.G, 1999, Quaternary Geology of Ohio: Ohio Division of Geological Survey, Map No. 2, scale 1:500,000</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1221</edomv>
                <edomvd>Whitfield, J.W., Ward, R.A., Denne, J.E., Holbrook, D.F., Bush, W.V., Lineback, J.A., Luza, K.V., Jensen, K.M., and Fishman, W.D., compilers, Richmond, G.M. and Weide, D.L., eds., 1994, Quaternary geologic map of the Ozark Plateau 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NJ-15), scale 1:1,000,000 [Bush, C.A., Digital edition, 2011], https://pubs.usgs.gov/imap/i-1420/nj-15/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1227</edomv>
                <edomvd>Copeland, C.W., Jr., Rheams, K.F., Neathery, T.L., Gilliland, W.A., Schmidt, Walter, Clark, W.C., Jr., and Pope, D.E., compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., eds., 1988, Quaternary geologic map of the Mobile 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NH-16), scale 1:1,000,000, [Bush, C.A., Digital edition, 2010], https://pubs.usgs.gov/imap/i-1420/nh-16/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1166</edomv>
                <edomvd>Lineback, J.A., 1979, Quaternary deposits of Illinois: Illinois State Geological Survey, scale 1:500,000.</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1134</edomv>
                <edomvd>Johnson, G.H., and Peebles, P.C., compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., and Bush, C.A., eds., 1986, Quaternary geologic map of the Hatteras 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NI-18), scale 1:1,000,000, [Bush, C.A., Digital edition, 2011], https://pubs.usgs.gov/imap/i-1420/ni-18/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1370</edomv>
                <edomvd>Moore, D.W., and Wermund, E.G, compilers; Moore, D.W., and Richmond, G.M., eds., 1993, Quaternary geologic map of the Monterrey 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NG-14), scale 1:1,000,000, [Bush, C.A., Digital edition, 2010], https://pubs.usgs.gov/imap/i-1420/ng-14/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1239</edomv>
                <edomvd>Farrand, W.R., Mickelson, D.M., Cowan, W.R., and Goebel, J.E., compilers; Richmond, G.M. and Fullerton, D.S., eds., 1984, Quaternary Geologic Map of the Lake Superior 4° x 6° Quadrangle, United States and Canada: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NL-16), scale 1:1,000,000, [Digital edition, 2002], https://pubs.usgs.gov/imap/i-1420/nl-16/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1173</edomv>
                <edomvd>Swinehart, J.B., Dreeszen, V.H., Richmond, G.M., Tipton, M.J., Bretz, Richard, Steece, F.V., Hallberg, G.R., and Goebel, J.E., compilers; Richmond, G.M., ed., 1994, Quaternary geologic map of the Platte River 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NK-14), scale 1:1,000,000, [Digital edition, 2008], https://pubs.usgs.gov/imap/i-1420/nk-14/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1128</edomv>
                <edomvd>Howard, A.D., Behling, R.E., Wheeler, W.H., Daniels, R.B., Swadley, W.C., Goldthwait, R.P., Fullerton, D.S., Sevon, W.D., Miller, R.A., compilers; Richmond, G.M., Fullerton, D.S., Christiansen, A.C., eds., 1991, Quaternary geologic map of the Blue Ridge 4° x 6° quadrangle, United States: Quaternary Geologic Atlas of the United States Map I-1420 (NJ-17), scale 1:1,000,000, [Bush, C.A., Digital edition, 2011], https://pubs.usgs.gov/imap/i-1420/nj-17/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1191</edomv>
                <edomvd>Pope, D.E., Gilliland, W.A., and Wermund, E.G., compilers; Richmond, G.M., Weide, D.L., and Moore, D.W., eds., 1990, Quaternary geologic map of the White Lake 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NH-15), scale 1:1,000,000 [Bush, C.A., Digital edition, 2012], https://pubs.usgs.gov/imap/i-1420/nh-15/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1376</edomv>
                <edomvd>Hartshorn, J.H., Thompson, W.B., Chapman, W.F., Black, R.F., Richmond, G.M., Grant, D.R., and Fullerton, D.S., compilers; Richmond, G.M. and Fullerton, D.S., eds., 1991, Quaternary Geologic Map of the Boston 4° x 6° Quadrangle, United States and Canada: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420(NK-19), scale 1:1,000,000, [Digital edition, 2006], https://pubs.usgs.gov/imap/i-1420/nk-19/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1185</edomv>
                <edomvd>Hallberg, G.R., Lineback, J.A., Mickelson, D.M., Knox, J.C., Goebel, J.E., Hobbs, H.C., Whitfield, J.W., Ward, R.A., Boellstorff, J.D., Swinehart, J.B., and Dreeszen, V.H., compilers; Richmond, G.M., Fullerton, D.S., and Christiansen, A.C., eds., 1994, Quaternary geologic map of the Des Moines 4° x 6° Quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NK-15), scale 1:1,000,000, [Digital edition, 2008], https://pubs.usgs.gov/imap/i-1420/nk-15/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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            <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>1160</edomv>
                <edomvd>Lineback, J.A., Bleuer, N.K., Mickelson, D.M., Ferrand, W.R., and Goldthwait, R.P., compilers; Richmond, G.M., and Fullerton, D.S., eds., 1983, Quaternary geologic map of the Chicago 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NK-16), scale 1:1,000,000, [Digital edition, 2002], https://pubs.usgs.gov/imap/i-1420/nk-16/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
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            <attrdomv>
              <edom>
                <edomv>1209</edomv>
                <edomvd>Goebel, J.E., Mickelson, D.M., Ferrand, W.R., Clayton, Lee, Knox, J.C., Cahow, Adam, Hobbs, H.C., Walton, M.S., compilers; Richmond, G.M. and Fullerton, D.S., eds., 1983, Quaternary Geologic Map of the Minneapolis 4° x 6° Quadrangle, United States: U.S. Geological Survey iscellaneous Investigations Series Map I-1420(NL-15), scale 1:1,000,000, [Digital edition, 2007], https://pubs.usgs.gov/imap/i-1420/nl-15/</edomvd>
                <edomvds>This report</edomvds>
              </edom>
            </attrdomv>
            <attrdomv>
              <edom>
                <edomv>1263</edomv>
                <edomvd>Richmond, G.M., Fullerton, D.S., and Weide, D.L., eds., Colquhoun, D.J., Friddell, M.S., Wheeler, W.H., Daniels, R.B., Gregory, J.P., Miller, R.A., and Van Nostrand, A.K., compilers; Richmond, G.M., Fullerton, D.S., Weide, D.L., eds., 1987, Quaternary geologic map of the Savannah 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NI-17), scale 1:1,000,000, [Bush, C.A., Digital edition, 2013], https://pubs.usgs.gov/imap/i-1420/ni-17/</edomvd>
                <edomvds>This report</edomvds>
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              <edom>
                <edomv>1203</edomv>
                <edomvd>Fullerton, D.S., Bluemle, L.C., Steece, F.V., Tipton, M.J., Bretz, Richard, and Goebel, J.E., compilers; Fullerton, D.S., ed., 1995, Quaternary geologic map of the Dakotas 4° x 6° quadrangle, United States: U.S. Geological Survey Miscellaneous Investigations Series Map I-1420 (NL-14), scale 1:1,000,000, [Bush, C.A., Digital edition, 2011], https://pubs.usgs.gov/imap/i-1420/nl-14/</edomvd>
                <edomvds>This report</edomvds>
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        <distliab>Any use of trade, product or firm names is for descriptive purposes only and does
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            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
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