<?xml version="1.0" encoding="UTF-8"?>
<metadata>
  <idinfo>
    <citation>
      <citeinfo>
        <origin>R.C. Orndorff</origin>
        <origin>R.J. McAleer</origin>
        <origin>E.A. Crider Jr</origin>
        <origin>G.J. Walsh</origin>
        <pubdate>20221101</pubdate>
        <title>Geologic Map of the Crown Point Quadrangle, Essex County, New York, and Addison County, Vermont</title>
        <geoform>vector digital data</geoform>
        <serinfo>
          <sername>Scientific Investigations Map</sername>
          <issue>3491</issue>
        </serinfo>
        <pubinfo>
          <pubplace>Reston, VA</pubplace>
          <publish>U.S. Geological Survey</publish>
        </pubinfo>
        <othercit>Walsh, G.J., Orndorff, R.C., and McAleer, R.J., 2022, Bedrock geologic map of the Crown Point quadrangle, Essex County, New York, and Addison County, Vermont: U.S. Geological Survey Scientific Investigations Map 3491, Scale 1:24,000, 1 sheet, includes 44-p. pamphlet.</othercit>
        <onlink>https://doi.org/10.3133/sim3491</onlink>
      </citeinfo>
    </citation>
    <descript>
      <abstract>The bedrock geology map database of the 7.5-minute Crown Point quadrangle consists of deformed and metamorphosed Mesoproterozoic gneisses of the Adirondack Highlands unconformably overlain by weakly deformed lower Paleozoic sedimentary rocks of the Champlain Valley. The Mesoproterozoic rocks occur on the eastern edge of the Adirondack Highlands and represent an extension of the Grenville Province of Laurentia. Granulite facies Mesoproterozoic paragneiss, marble, and amphibolite hosted the emplacement of granitic orthogneiss at approximately 1.18–1.15 giga-annum (Ga, billion years before present). The earliest of four phases of deformation (D1) is characterized by gneissosity, rarely preserved F1 isoclinal folds, and migmatite in the host rocks. Subsequent D2 deformation produced a composite penetrative gneissosity, migmatite, and isoclinal F2 folds. Towards the end of D2, felsic magmatism (including the regionally extensive Lyon Mountain Granite Gneiss, abbreviated "LMG") spread by penetrative migration as semiconcordant alkali feldspar granite sheets subparallel to S2 into previously deformed lithologies. The LMG crystallized at approximately 1.15 Ga and displays synkinematic F2 folds thus constraining the time of D2 deformation. Exhumation during D3 produced F3 folds exhibited in regional domes and basins, such as the Keeney Mountain synform, local reactivation of the S2 foliation, partial melting, metamorphism, metasomatism, iron ore remobilization, and intrusion of magnetite-bearing pegmatite both as layer-parallel sills and crosscutting dikes. D4 created NE- and NW-trending boudinage, local high-grade ductile shear zones, and crosscutting granitic pegmatite dikes. Kilometer (km)-scale lineaments readily observed in lidar data are Ediacaran mafic dikes and Phanerozoic brittle faults. The Paleozoic rocks are part of the Early Cambrian to Late Ordovician great American carbonate bank on the ancient margin of Laurentia. Cambrian-Ordovician stratigraphy records an approximately 1-km-thick section and a transition from synrift clastics to passive margin peritidal carbonate buildups to gradually deeper water subtidal to shelf carbonates during foreland basin development associated with the Taconic orogeny. The Paleozoic rocks are weakly folded and block faulted. Large areas of the Champlain Valley are covered by undifferentiated glacial deposits, some of which contain mapped landslides. The map also shows waste rock piles and tailings from historical mining operations and large areas of artificial fill.</abstract>
      <purpose>The geologic map database of the Crown Point quadrangle is intended to serve as a foundation for applying geologic information to problems involving land use decisions, groundwater availability and quality, earth resources such as natural aggregate for construction, assessment of natural hazards (earthquakes), and engineering and environmental studies for waste disposal sites and construction projects. The database and associated geologic map improves the understanding of the bedrock geology in the Adirondack Highlands, establishes a modern framework for 1:24,000-scale bedrock geologic mapping in the Adirondacks, provides a context for historical iron mines in the eastern Adirondacks, and updates the stratigraphy of the Champlain Valley in New York and Vermont.</purpose>
      <supplinf>CrownPointNY-VTSIM3491.gdb 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_FGDC1_Arc10.py, version of 29 March 2022.</supplinf>
    </descript>
    <timeperd>
      <timeinfo>
        <sngdate>
          <caldate>20221101</caldate>
        </sngdate>
      </timeinfo>
      <current>publication date</current>
    </timeperd>
    <status>
      <progress>Complete</progress>
      <update>None planned</update>
    </status>
	<spdom>
<bounding>
<westbc>-73.5000</westbc>
<eastbc>-73.3650</eastbc>
<northbc>44.0000</northbc>
<southbc>43.8750</southbc>
</bounding>
</spdom>
    <keywords>
      <theme>
        <themekt>Geologic Names</themekt>
        <themekey>Iberville Formation</themekey>
        <themekey>Potsdam Sandstone</themekey>
        <themekey>Stony Point Formation</themekey>
        <themekey>Ticonderoga Formation</themekey>
        <themekey>Orwell Limestone</themekey>
        <themekey>Whitehall Formation</themekey>
        <themekey>Providence Island Dolomite</themekey>
        <themekey>Fort Cassin Formation</themekey>
        <themekey>Cutting Dolomite</themekey>
        <themekey>Glens Falls Limestone</themekey>
        <themekey>Lyon Mountain Granite Gneiss</themekey>
        <themekey>Valcour Limestone</themekey>
        <themekey>Crown Point Limestone</themekey>
      </theme>
      <theme>
        <themekt>USGS Thesaurus</themekt>
        <themekey>geologic maps</themekey>
        <themekey>deformation (geologic)</themekey>
        <themekey>metamorphic rocks</themekey>
        <themekey>surficial geologic units</themekey>
        <themekey>maps and atlases</themekey>
        <themekey>fracture (geologic)</themekey>
        <themekey>structural geology</themekey>
        <themekey>Neoproterozoic</themekey>
        <themekey>uplift</themekey>
        <themekey>igneous rocks</themekey>
        <themekey>geologic structure</themekey>
        <themekey>Quaternary</themekey>
        <themekey>geologic contacts</themekey>
        <themekey>faulting (geologic)</themekey>
        <themekey>Mesoproterozoic</themekey>
        <themekey>conodonts</themekey>
        <themekey>Cambrian</themekey>
        <themekey>alteration</themekey>
        <themekey>geologic history</themekey>
        <themekey>unconsolidated deposits</themekey>
        <themekey>lineation (geologic)</themekey>
        <themekey>Paleozoic</themekey>
        <themekey>mineral resources</themekey>
        <themekey>economic geology</themekey>
        <themekey>tectonic processes</themekey>
        <themekey>geologic time periods</themekey>
        <themekey>Ordovician</themekey>
        <themekey>geologic time scales</themekey>
        <themekey>stratigraphy</themekey>
        <themekey>Holocene</themekey>
        <themekey>metamorphism (geological)</themekey>
        <themekey>mineral deposits</themekey>
        <themekey>hazards</themekey>
        <themekey>landslides</themekey>
        <themekey>Proterozoic</themekey>
        <themekey>fossils</themekey>
        <themekey>building stone resources</themekey>
        <themekey>mine waste</themekey>
        <themekey>folding (geologic)</themekey>
        <themekey>bedrock geologic units</themekey>
        <themekey>sedimentary rocks</themekey>
        <themekey>geologic processes</themekey>
      </theme>
      <theme>
        <themekt>Lithologic classification of geologic map units</themekt>
        <themekey>Syenite</themekey>
        <themekey>Amphibolite</themekey>
        <themekey>Metavolcanic rock</themekey>
        <themekey>Tectonic breccia</themekey>
        <themekey>Pegmatite</themekey>
        <themekey>Paragneiss</themekey>
        <themekey>Calc-silicate rock</themekey>
        <themekey>Sedimentary rock</themekey>
        <themekey>Plutonic rock</themekey>
        <themekey>Limestone</themekey>
        <themekey>Alluvium</themekey>
        <themekey>Diabase</themekey>
        <themekey>Cataclasite</themekey>
        <themekey>Landslide</themekey>
        <themekey>Clastic rock</themekey>
        <themekey>Till</themekey>
        <themekey>Granitic gneiss</themekey>
        <themekey>Mixed carbonate/clastic rock</themekey>
        <themekey>Migmatite</themekey>
        <themekey>Quartz syenite</themekey>
        <themekey>Carbonate rock</themekey>
        <themekey>Alkali-feldspar granite</themekey>
        <themekey>Granofels</themekey>
        <themekey>Marble</themekey>
        <themekey>Dolostone</themekey>
        <themekey>Augen gneiss</themekey>
        <themekey>Sandstone</themekey>
        <themekey>Metasedimentary rock</themekey>
        <themekey>Shale</themekey>
        <themekey>Conglomerate</themekey>
        <themekey>Metamorphic rock</themekey>
        <themekey>Gneiss</themekey>
        <themekey>Quartzite</themekey>
        <themekey>Delta</themekey>
      </theme>
      <theme>
        <themekt>ISO 19115 Topic Category</themekt>
        <themekey>environment</themekey>
        <themekey>utilitiesCommunication</themekey>
        <themekey>geoscientificInformation</themekey>
        <themekey>economy</themekey>
      </theme>
      <theme>
        <themekt>ISO 19115 Topic Categories</themekt>
        <themekey>structure</themekey>
        <themekey>utilitiesCommunication</themekey>
        <themekey>economy</themekey>
        <themekey>environment</themekey>
        <themekey>geoscientificInformation</themekey>
      </theme>
      <theme>
        <themekt>USGS Metadata Identifier</themekt>
        <themekey>USGS:dcf77dd6-6cd5-488d-addd-071628589098</themekey>
      </theme>
      <place>
        <placekt>Common Geographic Names</placekt>
        <placekey>United States</placekey>
        <placekey>Vermont</placekey>
        <placekey>Addison</placekey>
        <placekey>Ticonderoga</placekey>
        <placekey>New York</placekey>
        <placekey>Crown Point</placekey>
        <placekey>Essex</placekey>
      </place>
    </keywords>
    <accconst>None. Acknowledgment of the U.S. Geological Survey would be appreciated in products derived from these data.</accconst>
    <useconst>None. Acknowledgment of the U.S. Geological Survey would be appreciated in products derived from these data. Although software enables the user to display images at various scales, map data in this report should not be used at scales greater than 1:24,000.</useconst>
    <ptcontac>
      <cntinfo>
        <cntorgp>
          <cntorg>U.S. Geological Survey, Northeast Region</cntorg>
          <cntper>Ernest A Crider</cntper>
        </cntorgp>
        <cntpos>Geologist</cntpos>
        <cntaddr>
          <addrtype>mailing</addrtype>
          <address>Mail Stop 926A, 12201 Sunrise Valley Dr</address>
          <city>Reston</city>
          <state>VA</state>
          <postal>20192</postal>
          <country>US</country>
        </cntaddr>
        <cntvoice>703-648-6906</cntvoice>
        <cntfax>703-648-6953</cntfax>
        <cntemail>ecrider@usgs.gov</cntemail>
      </cntinfo>
    </ptcontac>
    <datacred>Funding for this report was provided by the National Cooperative Geologic Mapping Program (NCGMP) from 2016 to 2022. Additional support and cooperation was provided by the State of Vermont, Vermont Agency of Natural Resources, Vermont Geological Survey and the State of New York, Department of Education, New York Geological Survey.</datacred>
    <native>MS Windows Version 6.2 (Build 9200); Esri ArcGIS 10.8.1.14362</native>
  </idinfo>
  <dataqual>
    <attracc>
      <attraccr>Geologic contacts and information were garnered from 1:24,000-scale mapping of geologic material based on observation from fieldwork, previously published geologic maps, and unpublished geologic data in the region. The geologic information might change if additional outcrops are discovered or exposed as the natural land changes, or as the result of development, or advances in scientific research are made. The features in the database are not based on legal parcels or definitions. Users of this data should pay close attention to the references in the pamphlet for the published geologic map as sources relevant to the database may not be included in the DataSources table of this database. Confidence that an individual feature exists and confidence that a feature is correctly identified are described in per-feature attributes of the ExistenceConfidence and IdentityConfidence fields.</attraccr>
    </attracc>
    <logic>Geologic contacts and information were garnered from 1:24,000-scale mapping of bedrock and surficial material based on observation from and geologic fieldwork in the region. The geologic information might change if additional outcrops are discovered or exposed as the natural land changes or as the result of development. The features in the database are not based on legal parcels or definitions. Topology tests were performed to ensure the integrity of the data. These tests checked for polygon overlaps and gaps and line pseudos, dangles, and intersections. Additional tests were conducted to ensure that linework from geologic contacts match polygon boundaries where necessary. Database verifies as level 3 compliant under the "GeMS" schema. Level 3 compliance was achieved by deleting references used for the publication of the geologic map and pamphlet. A MapUnitOverlayLines feature class exists to match the surficial polygons in the MapUnitOverlayPolys feature class.</logic>
    <complete>Dataset is considered complete for the information presented, as described in the abstract. Users are advised to read the rest of the metadata record carefully for additional details.</complete>
    <posacc>
      <horizpa>
        <horizpar>Data were delineated on classic U.S. Geological Survey (USGS) 7.5-minute topographic maps at 1:24,000 scale. Therefore, the horizontal accuracy is assumed to be within National Map Accuracy Standards, with a horizontal accuracy of 45.6 feet at the 95% confidence level. In addition, the horizontal accuracy standard requires that the positions of 90 percent of all points tested must be accurate within 1/50th of an inch (0.05 centimeters) on the map. For more information see U.S. Geological Survey Fact Sheet 171-99. Horizontal estimated accuracy of individual features within this database is given on a per-feature basis by the LocationConfidenceMeters field. Values are expected to be correct within a factor of 2.</horizpar>
      </horizpa>
      <vertacc>
        <vertaccr>The data were delineated on classic U.S. Geological Survey (USGS) 7.5-minute topographic maps at 1:24,000 scale. Therefore, the vertical accuracy is assumed to be within National Map Accuracy Standards, with a vertical accuracy of 11.9 feet at the 95% confidence level. In addition, the vertical accuracy standard requires that the elevation of 90 percent of all points tested much be correct within half of the contour interval. For more information see U.S. Geological Survey Fact Sheet 171-99.</vertaccr>
      </vertacc>
    </posacc>
    <lineage>
      <srcinfo>
        <srccite>
          <citeinfo>
            <origin>J.M. Hanchar</origin>
            <origin>P.M. Valley</origin>
            <origin>M.J. Whitehouse</origin>
            <pubdate>20110401</pubdate>
            <title>New insights on the evolution of the Lyon Mountain Granite and associated Kiruna-type magnetite-apatite deposits, Adirondack Mountains, New York State</title>
            <geoform>publication</geoform>
            <serinfo>
              <sername>Geosphere</sername>
              <issue>v. 7, no. 2</issue>
            </serinfo>
            <pubinfo>
              <pubplace>unknown</pubplace>
              <publish>Geological Society of America</publish>
            </pubinfo>
            <othercit>Valley, P.M., Hanchar, J.M., and Whitehouse, M.J., 2011, New insights on the evolution of the Lyon Mountain Granite and associated Kiruna-type magnetite-apatite deposits, Adirondack Mountains, New York State: Geosphere, v. 7, no. 2, p. 357–389.</othercit>
            <onlink>https://doi.org/10.1130/GES00624.1</onlink>
          </citeinfo>
        </srccite>
        <typesrc>hardcopy</typesrc>
        <srctime>
          <timeinfo>
            <sngdate>
              <caldate>20110401</caldate>
            </sngdate>
          </timeinfo>
          <srccurr>publication date</srccurr>
        </srctime>
        <srccitea>DASCPNYVT123</srccitea>
        <srccontr>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, or the additional supporting structural and cartographic information.</srccontr>
      </srcinfo>
      <srcinfo>
        <srccite>
          <citeinfo>
            <origin>G.J. Walsh</origin>
            <origin>M. Toft</origin>
            <origin>M.L. Williams</origin>
            <origin>S.P. Regan</origin>
            <origin>R. McAleer</origin>
            <origin>J.R. Chiarenzelli</origin>
            <pubdate>20190508</pubdate>
            <title>Syn-collisional exhumation of hot middle crust in the Adirondack Mountains New York, USA—Implications for extensional orogenesis in the southern Grenville province</title>
            <geoform>publication</geoform>
            <serinfo>
              <sername>Geosphere</sername>
              <issue>v. 15, no. 4</issue>
            </serinfo>
            <pubinfo>
              <pubplace>unknown</pubplace>
              <publish>Geological Society of America</publish>
            </pubinfo>
            <othercit>Regan, S.P., Walsh, G.J., Williams, M.L., Chiarenzelli, J.R., Toft, M., and McAleer, R., 2019a, Syn-collisional exhumation of hot middle crust in the Adirondack Mountains (New York, USA)—Implications for extensional orogenesis in the southern Grenville province: Geosphere, v. 15, no. 4, p. 1240–1261.</othercit>
            <onlink>https://doi.org/10.1130/GES02029.1</onlink>
          </citeinfo>
        </srccite>
        <typesrc>hardcopy</typesrc>
        <srctime>
          <timeinfo>
            <sngdate>
              <caldate>20190508</caldate>
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          <srccurr>publication date</srccurr>
        </srctime>
        <srccitea>DASCPNYVT097</srccitea>
        <srccontr>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, or the additional supporting structural and cartographic information.</srccontr>
      </srcinfo>
      <srcinfo>
        <srccite>
          <citeinfo>
            <origin>L. Tan</origin>
            <pubdate>19661101</pubdate>
            <title>Major pegmatite deposits of New York State</title>
            <geoform>publication</geoform>
            <serinfo>
              <sername>New York State Museum Bulletin</sername>
              <issue>408</issue>
            </serinfo>
            <pubinfo>
              <pubplace>Albany, NY</pubplace>
              <publish>The University of the State of New York</publish>
            </pubinfo>
            <othercit>Tan, L., 1966, Major pegmatite deposits of New York State: New York State Museum Bulletin 408, 138 p.</othercit>
          </citeinfo>
        </srccite>
        <typesrc>hardcopy</typesrc>
        <srctime>
          <timeinfo>
            <sngdate>
              <caldate>19661101</caldate>
            </sngdate>
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          <srccurr>publication date</srccurr>
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        <srccitea>DASCPNYVT118</srccitea>
        <srccontr>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, or the additional supporting structural and cartographic information.</srccontr>
      </srcinfo>
      <srcinfo>
        <srccite>
          <citeinfo>
            <origin>J. Rodgers</origin>
            <pubdate>19371101</pubdate>
            <title>Stratigraphy and structure in the Upper Champlain Valley</title>
            <geoform>publication</geoform>
            <serinfo>
              <sername>Bulletin</sername>
              <issue>v. 48, no. 11</issue>
            </serinfo>
            <pubinfo>
              <pubplace>unknown</pubplace>
              <publish>Geological Society of America</publish>
            </pubinfo>
            <othercit>Rodgers, J., 1937, Stratigraphy and structure in the Upper Champlain Valley: Geological Society of American Bulletin, v. 48, no. 11, p. 1573–1588.</othercit>
            <onlink>https://doi.org/10.1130/GSAB-48-1573</onlink>
          </citeinfo>
        </srccite>
        <typesrc>hardcopy</typesrc>
        <srctime>
          <timeinfo>
            <sngdate>
              <caldate>19371101</caldate>
            </sngdate>
          </timeinfo>
          <srccurr>publication date</srccurr>
        </srctime>
        <srccitea>DASCPNYVT104</srccitea>
        <srccontr>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, or the additional supporting structural and cartographic information.</srccontr>
      </srcinfo>
      <srcinfo>
        <srccite>
          <citeinfo>
            <origin>G.J. Walsh</origin>
            <origin>N.M. Ratcliffe</origin>
            <origin>P.J. Thompson</origin>
            <origin>M.H. Gale</origin>
            <origin>R.S. Stanley</origin>
            <pubdate>20110101</pubdate>
            <title>Bedrock geologic map of Vermont</title>
            <geoform>publication</geoform>
            <serinfo>
              <sername>Scientific Investigations Map</sername>
              <issue>3184</issue>
            </serinfo>
            <pubinfo>
              <pubplace>Reston, VA</pubplace>
              <publish>U.S. Geological Survey</publish>
            </pubinfo>
            <othercit>Ratcliffe, N.M., Stanley, R.S., Gale, M.H., Thompson, P.J., and Walsh, G.J., 2011, Bedrock geologic map of Vermont: U.S. Geological Survey Scientific Investigations Map 3184, 1 sheet, scale 1:100,000.</othercit>
            <onlink>https://doi.org/10.3133/sim3184</onlink>
          </citeinfo>
        </srccite>
        <srcscale>100000</srcscale>
        <typesrc>hardcopy</typesrc>
        <srctime>
          <timeinfo>
            <sngdate>
              <caldate>20110101</caldate>
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          <srccurr>publication date</srccurr>
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        <srccitea>DASCPNYVT092</srccitea>
        <srccontr>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, or the additional supporting structural and cartographic information.</srccontr>
      </srcinfo>
      <srcinfo>
        <srccite>
          <citeinfo>
            <origin>S.P. Regan</origin>
            <origin>K.A. Suarez</origin>
            <origin>M.L. Williams</origin>
            <origin>C.R. Pless</origin>
            <origin>G.B. Baird</origin>
            <origin>T.W. Grover</origin>
            <pubdate>20181014</pubdate>
            <title>Migmatites of the eastern Adirondack Mountains—New constraints on the timing, petrology, and tectonic setting of partial melting</title>
            <geoform>publication</geoform>
            <pubinfo>
              <pubplace>Castleton, VT</pubplace>
              <publish>unknown</publish>
            </pubinfo>
            <othercit>Williams, M.L., Grover, T.W., Pless, C.R., Suarez, K.A., Regan, S.P., and Baird, G.B., 2018, Migmatites of the eastern Adirondack Mountains—New constraints on the timing, petrology, and tectonic setting of partial melting, Trip A–1, in Grover, T.W., and Mango, H., eds., Guidebook for field trips in New York and Vermont: New England Intercollegiate Geological Conference, 110th Annual Meeting, and New York State Geological Association, 90th Annual Meeting, Castleton, Vt., Oct. 12–14, 2018, Field Trip Guidebook, Castleton, Vt., Castleton University, p. A1–1 to A1–34.</othercit>
            <onlink>https://castleton.s3.amazonaws.com/files/pages/a1-final.pdf</onlink>
          </citeinfo>
        </srccite>
        <typesrc>hardcopy</typesrc>
        <srctime>
          <timeinfo>
            <sngdate>
              <caldate>20181014</caldate>
            </sngdate>
          </timeinfo>
          <srccurr>publication date</srccurr>
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        <srccitea>DASCPNYVT136</srccitea>
        <srccontr>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, or the additional supporting structural and cartographic information.</srccontr>
      </srcinfo>
      <srcinfo>
        <srccite>
          <citeinfo>
            <origin>U.S. Geological Survey, Science Publishing Network (SPN)</origin>
            <origin>U.S. Geological Survey (USGS)</origin>
            <pubdate>20150101</pubdate>
            <title>U.S. Geological Survey Science Publishing Network, MapStyleGuide_DMU_print_1sht_v1-1_01-15.pdf.</title>
            <geoform>publication</geoform>
            <pubinfo>
              <pubplace>Reston, VA</pubplace>
              <publish>U.S. Geological Survey (USGS)</publish>
            </pubinfo>
            <othercit>U.S. Geological Survey Science Publishing Network, MapStyleGuide_DMU_print_1sht_v1-1_01-15.pdf.</othercit>
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              <caldate>20150101</caldate>
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          <srccurr>publication date</srccurr>
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        <srccitea>USGS</srccitea>
        <srccontr>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, or the additional supporting structural and cartographic information.</srccontr>
      </srcinfo>
      <srcinfo>
        <srccite>
          <citeinfo>
            <origin>H.L. Alling</origin>
            <pubdate>19180614</pubdate>
            <title>The Adirondack graphite deposits</title>
            <geoform>publication</geoform>
            <serinfo>
              <sername>New York State Museum Bulletin</sername>
              <issue>199</issue>
            </serinfo>
            <pubinfo>
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            <title>Bedrock geologic map of the Crown Point quadrangle, Essex County, New York, and Addison County, Vermont</title>
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            <serinfo>
              <sername>Scientific Investigations Map</sername>
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              <publish>U.S. Geological Survey</publish>
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            <othercit>This report, Walsh, G.J., Orndorff, R.C., and McAleer, R.J., 2022, Bedrock geologic map of the Crown Point quadrangle, Essex County, New York, and Addison County, Vermont: U.S. Geological Survey Scientific Investigations Map 3491, Scale 1:24,000, 1 sheet, includes 44-p. pamphlet.</othercit>
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            <origin>P.M. Valley</origin>
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              <pubplace>Plattsburgh, N.Y</pubplace>
              <publish>State University of New York</publish>
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            <serinfo>
              <sername>Geology</sername>
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              <sername>Professional Paper</sername>
              <issue>237</issue>
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            <title>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.</title>
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              <sername>Open-File Report</sername>
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            <serinfo>
              <sername>Open-File Reports</sername>
              <issue>1g066.4, 1g066.6, 1g234, and 1g13798</issue>
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            <origin>U.S. Geological Survey (USGS)</origin>
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        <srccontr>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, or the additional supporting structural and cartographic information.</srccontr>
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              <caldate>20130131</caldate>
            </sngdate>
          </timeinfo>
          <srccurr>publication date</srccurr>
        </srctime>
        <srccitea>DASCPNYVT066</srccitea>
        <srccontr>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, or the additional supporting structural and cartographic information.</srccontr>
      </srcinfo>
      <srcinfo>
        <srccite>
          <citeinfo>
            <origin>D.H. Newland</origin>
            <origin>J.R. Kemp</origin>
            <pubdate>19071207</pubdate>
            <title>Geology of the Adirondack magnetic iron ores, with a report on the Mineville-Port Henry mine group</title>
            <geoform>publication</geoform>
            <serinfo>
              <sername>New York State Museum Bulletin</sername>
              <issue>119</issue>
            </serinfo>
            <pubinfo>
              <pubplace>Albany, NY</pubplace>
              <publish>The University of the State of New York</publish>
            </pubinfo>
            <othercit>Newland, D.H., and Kemp, J.F., 1908, Geology of the Adirondack magnetic iron ores, with a report on the Mineville-Port Henry mine group: New York State Museum Bulletin 119, 182 p.</othercit>
          </citeinfo>
        </srccite>
        <typesrc>hardcopy</typesrc>
        <srctime>
          <timeinfo>
            <sngdate>
              <caldate>19071207</caldate>
            </sngdate>
          </timeinfo>
          <srccurr>publication date</srccurr>
        </srctime>
        <srccitea>DASCPNYVT081</srccitea>
        <srccontr>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, or the additional supporting structural and cartographic information.</srccontr>
      </srcinfo>
      <srcinfo>
        <srccite>
          <citeinfo>
            <origin>C.W. Welby</origin>
            <pubdate>19610101</pubdate>
            <title>Bedrock geology of the central Champlain Valley of Vermont</title>
            <geoform>publication</geoform>
            <serinfo>
              <sername>Bulletin</sername>
              <issue>14</issue>
            </serinfo>
            <pubinfo>
              <pubplace>Montpelier, VT</pubplace>
              <publish>Vermont Geological Survey</publish>
            </pubinfo>
            <othercit>Welby, C.W., 1961, Bedrock geology of the central Champlain Valley of Vermont: Vermont Geological Survey Bulletin 14, 296 p., 13 pls., pl. 1 map scale 1:62,500.</othercit>
          </citeinfo>
        </srccite>
        <srcscale>62500</srcscale>
        <typesrc>hardcopy</typesrc>
        <srctime>
          <timeinfo>
            <sngdate>
              <caldate>19610101</caldate>
            </sngdate>
          </timeinfo>
          <srccurr>publication date</srccurr>
        </srctime>
        <srccitea>DASCPNYVT130</srccitea>
        <srccontr>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, or the additional supporting structural and cartographic information.</srccontr>
      </srcinfo>
      <procstep>
        <procdesc>The base map was downloaded from http://gis.ny.gov/gisdata/quads/drg24/i51.htm. Separations were cleaned of scratches in Adobe Photoshop and registered and rectified in ArcGIS ArcMap 10.6. The hydrologic water boundary information was extracted from the cultural layer as a separate raster using ArcGIS ArcScan and removed from the cultural layer leaving only transportation, geographic, and hydrologic names. Water boundaries were vectorized using ArcGIS ArcScan and left in a shapefile to be used for concealing bedrock contacts. The boundaries of Lake Champlain were extracted directly from modern LiDAR and placed into the water separate. A vector polygon of Lake Champlain is added to the MapUnitOverlayPolys feature class because much of the surficial information and some bedrock information shares a contact with the boundaries of Lake Champlain. Topographic, hydrologic, and cultural information from the adjoining Bridport, Vermont, quadrangle were manually added onto the New York State base map in the southeast corner of the map using ArcGIS ArcScan.</procdesc>
        <procdate>20200624</procdate>
        <proccont>
          <cntinfo>
            <cntorgp>
              <cntorg>U.S. Geological Survey, Northeast Region</cntorg>
              <cntper>Ernest A Crider</cntper>
            </cntorgp>
            <cntpos>Geologist</cntpos>
            <cntaddr>
              <addrtype>mailing</addrtype>
              <address>Mail Stop 926A, 12201 Sunrise Valley Dr</address>
              <city>Reston</city>
              <state>VA</state>
              <postal>20192</postal>
              <country>US</country>
            </cntaddr>
            <cntvoice>703-648-6906</cntvoice>
            <cntfax>703-648-6953</cntfax>
            <cntemail>ecrider@usgs.gov</cntemail>
          </cntinfo>
        </proccont>
      </procstep>
      <procstep>
        <procdesc>Geologic data was delivered from the scientist as geodatabase features classes. Line feature classes including ContactsandFaults, MapUnitOverlayLines, and Geologic Lines were smoothed and generalized in ArcGIS ArcMap 10.6. Linework was then loaded into a new "GeMS" compliant database. The smoothed lines were used to create MapUnitPolys and MapUnitOverlayPolys. Polygons were reattributed manually. OrientationPoint data was carefully vetted for quality to ensure structural data was sound. Outcrop and areas of radiation polygons in the OverlayPolys feature class were smoothed or enlarged and in some cases merged where overlapping. Mine locations, area of radiation (point), conodont data, and geochronologic information was extracted from the OrientationPoints feature class into the GeochronPoints, GenericPoints, and FossilPoints feature classes. Station data, geologic points containing no structural measurements, were placed into the "Stations" feature class. Cartographic representations in ArcGIS ArcMap were used to symbolize the geologic map using FGDC geologic map standards. Labels were placed using individual annotation features classes and later merged into "GeologicMapAnno" annotation class for publication of the database.</procdesc>
        <procdate>20201202</procdate>
      </procstep>
      <procstep>
        <procdesc>Following edit, reference data was placed into the DataSources object class. Edited description of map units was added into the DescriptionOfMapUnits object class, and the hierarchy key was completed. The glossary was completed with as much of the edited explanation of map symbols from the published geologic map as possible. Database validation was used to remove extraneous datasources. The database validates to level 3.</procdesc>
        <procdate>20220909</procdate>
        <proccont>
          <cntinfo>
            <cntorgp>
              <cntorg>U.S. Geological Survey, Northeast Region</cntorg>
              <cntper>Ernest A Crider</cntper>
            </cntorgp>
            <cntpos>Geologist</cntpos>
            <cntaddr>
              <addrtype>mailing</addrtype>
              <address>Mail Stop 926A, 12201 Sunrise Valley Dr</address>
              <city>Reston</city>
              <state>VA</state>
              <postal>20192</postal>
              <country>US</country>
            </cntaddr>
            <cntvoice>703-648-6906</cntvoice>
            <cntfax>703-648-6953</cntfax>
            <cntemail>ecrider@usgs.gov</cntemail>
          </cntinfo>
        </proccont>
      </procstep>
    </lineage>
  </dataqual>
  <eainfo>
    <overview>
      <eaover>Database CrownPointNY-VTSIM3491.gdb contains the following elements: non-spatial table DescriptionOfMapUnits (47 rows); non-spatial table DataSources (26 rows); non-spatial table Glossary (66 rows); non-spatial table GeoMaterialDict (101 rows); feature dataset GeologicMap which contains feature class MapUnitPolys (370 features), feature class DataSourcePolys (0 features), feature class MapUnitOverlayPolys (70 features), feature class OverlayPolys (2728 features), feature class ContactsAndFaults (766 features), feature class GeologicLines (11 features), feature class CartographicLines (4 features), feature class IsoValueLines (0 features), feature class OrientationPoints (4374 features), feature class GeochronPoints (12 features), feature class FossilPoints (5 features), feature class Stations (1421 features), feature class GenericPoints (69 features), feature class MapUnitOverlayLines (175 features), and feature class GeologicMapAnno (1908 features); feature dataset CorrelationOfMapUnits which contains feature class CMUMapUnitPolys (39 features), feature class CMULines (64 features), and feature class CMUPoints (32 features).</eaover>
      <eadetcit>Detailed descriptions of entities, attributes, and attribute values are given in metadata for constituent elements of the database. See also "GeMS (Geologic Map Schema)--a standard format for the digital publication of geologic maps", available at http://ngmdb.usgs.gov/Info/standards/GeMS/.</eadetcit>
    </overview>
  </eainfo>
  <distinfo>
    <distrib>
      <cntinfo>
        <cntorgp>
          <cntorg>U.S. Geological Survey</cntorg>
          <cntper>National Geologic Map Database</cntper>
        </cntorgp>
        <cntaddr>
          <addrtype>mailing</addrtype>
          <address>Denver Federal Center, Building 810, Mail Stop 302</address>
          <city>Denver</city>
          <state>CO</state>
          <postal>80225</postal>
          <country>US</country>
        </cntaddr>
        <cntvoice>1-888-275-8747</cntvoice>
        <cntemail>ngmdb@usgs.gov</cntemail>
      </cntinfo>
    </distrib>
    <distliab>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.</distliab>
    <stdorder>
      <digform>
        <digtinfo>
          <formname>Digital Data</formname>
        </digtinfo>
        <digtopt>
          <onlinopt>
            <computer>
              <networka>
                <networkr>https://doi.org/10.3133/sim3491</networkr>
              </networka>
            </computer>
          </onlinopt>
        </digtopt>
      </digform>
      <fees>None</fees>
    </stdorder>
  </distinfo>
  <metainfo>
    <metd>20240410</metd>
    <metc>
      <cntinfo>
        <cntorgp>
          <cntorg>U.S. Geological Survey, Northeast Region</cntorg>
          <cntper>Ernest A Crider</cntper>
        </cntorgp>
        <cntpos>Geologist</cntpos>
        <cntaddr>
          <addrtype>mailing</addrtype>
          <address>Mail Stop 926A, 12201 Sunrise Valley Dr</address>
          <city>Reston</city>
          <state>VA</state>
          <postal>20192</postal>
          <country>US</country>
        </cntaddr>
        <cntvoice>703-648-6906</cntvoice>
        <cntfax>703-648-6953</cntfax>
        <cntemail>ecrider@usgs.gov</cntemail>
      </cntinfo>
    </metc>
    <metstdn>FGDC Content Standard for Digital Geospatial Metadata</metstdn>
    <metstdv>FGDC-STD-001-1998</metstdv>
    <mettc>local time</mettc>
  </metainfo>
</metadata>
