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<mdChar>
<CharSetCd value="004">
</CharSetCd>
</mdChar>
<mdHrLv>
<ScopeCd value="005">
</ScopeCd>
</mdHrLv>
<mdContact>
<rpOrgName>Wyoming State Geological Survey</rpOrgName>
<rpCntInfo>
<cntPhone>
<voiceNum>307-745-2250</voiceNum>
</cntPhone>
<cntAddress addressType="postal">
<delPoint>PO Box 1347</delPoint>
<city>Laramie</city>
<adminArea>WY</adminArea>
<postCode>82073</postCode>
<country>US</country>
<eMailAdd>wsgs-info@wyo.gov</eMailAdd>
</cntAddress>
<cntHours>M-F 8 am - 5 pm Mountain Time</cntHours>
</rpCntInfo>
<role>
<RoleCd value="007">
</RoleCd>
</role>
</mdContact>
<mdDateSt>20250101</mdDateSt>
<mdStanName>ArcGIS Metadata</mdStanName>
<mdStanVer>1.0</mdStanVer>
<distInfo>
<distributor>
<distorCont>
<rpOrgName>Wyoming State Geological Survey</rpOrgName>
<rpCntInfo>
<cntPhone>
<voiceNum>307-745-2250</voiceNum>
</cntPhone>
<cntAddress addressType="postal">
<delPoint>PO Box 1347</delPoint>
<city>Laramie</city>
<adminArea>WY</adminArea>
<postCode>82073</postCode>
<country>US</country>
<eMailAdd>wsgs-info@wyo.gov</eMailAdd>
</cntAddress>
<cntHours>M-F 8 am - 5 pm Mountain Time</cntHours>
</rpCntInfo>
<role>
<RoleCd value="005">
</RoleCd>
</role>
</distorCont>
<distorOrdPrc>
<resFees>None</resFees>
</distorOrdPrc>
<distorFormat>
<formatName>ArcGIS File Geodatabase</formatName>
</distorFormat>
<distorTran>
<onLineSrc>
<linkage>withheld</linkage>
</onLineSrc>
</distorTran>
</distributor>
<distTranOps>
<onLineSrc>
<linkage>https://doi.org/10.15786/wyoscholar/10111</linkage>
</onLineSrc>
</distTranOps>
</distInfo>
<dataIdInfo>
<idCitation>
<resTitle>Cheyenne 100k Bedrock Geologic Map</resTitle>
<date>
<pubDate>2025-01-01</pubDate>
</date>
<citRespParty>
<rpOrgName>Wyoming State Geological Survey</rpOrgName>
<role>
<RoleCd value="006">
</RoleCd>
</role>
</citRespParty>
<citRespParty>
<rpOrgName>Wyoming State Geological Survey</rpOrgName>
<rpCntInfo>
<cntAddress>
<delPoint>Laramie, WY</delPoint>
</cntAddress>
</rpCntInfo>
<role>
<RoleCd value="010">
</RoleCd>
</role>
</citRespParty>
<presForm>
<PresFormCd value="005">
</PresFormCd>
</presForm>
<presForm>
<fgdcGeoform>vector digital data</fgdcGeoform>
</presForm>
<datasetSeries>
<seriesName>Data Release</seriesName>
<issId>2025-30</issId>
</datasetSeries>
<otherCitDet>Suggested citation:
Wyoming State Geological Survey, 2025, Digital data for the geologic map of the Cheyenne 30' x 60' quadrangle, Wyoming: Wyoming State Geological Survey Data Release 2025-30, scale 1:100,000, https://doi.org/10.15786/wyoscholar/10111.
Original map publication:
Ver Ploeg, A.J., 1995, Geologic map of the Cheyenne 30’ x 60’ quadrangle, southeastern Wyoming, western Nebraska, and northern Colorado: Wyoming State Geological Survey Map Series 46, scale 1:100,000.</otherCitDet>
<collTitle>Geologic map of the Cheyenne 30’ x 60’ quadrangle, southeastern Wyoming, western Nebraska, and northern Colorado</collTitle>
</idCitation>
<idAbs>This digital database contains information used to publish the 1:100,000-scale geologic map of the Cheyenne quadrangle, Wyoming.</idAbs>
<idPurp>The bedrock geologic map of the Cheyenne, Wyoming 1:100,000 quadrangle was developed to provide regional scale geologic mapping for city and county planning, industrial and mineral development, and general public use. This dataset is a conversion of previously published map data to conform to GeMS (Geologic Map Schema)--a standard format for the digital publication of geologic maps--and is GeMS Level 3 compliant. The objective of the data conversion is to reproduce the original published mapping with little to no added interpretation.</idPurp>
<idCredit>Wyoming State Geological Survey</idCredit>
<idStatus>
<ProgCd value="001">
</ProgCd>
</idStatus>
<idPoC>
<rpOrgName>Wyoming State Geological Survey</rpOrgName>
<rpCntInfo>
<cntPhone>
<voiceNum>307-745-2250</voiceNum>
</cntPhone>
<cntAddress addressType="postal">
<delPoint>PO Box 1347</delPoint>
<city>Laramie</city>
<adminArea>WY</adminArea>
<postCode>82073</postCode>
<country>US</country>
<eMailAdd>wsgs-info@wyo.gov</eMailAdd>
</cntAddress>
<cntHours>M-F 8 am - 5 pm Mountain Time</cntHours>
</rpCntInfo>
<role>
<RoleCd value="007">
</RoleCd>
</role>
</idPoC>
<resMaint>
<maintFreq>
<MaintFreqCd value="011">
</MaintFreqCd>
</maintFreq>
</resMaint>
<placeKeys>
<keyword>Cheyenne</keyword>
<keyword>Wyoming</keyword>
</placeKeys>
<themeKeys>
<keyword>geoscientificInformation</keyword>
<thesaName>
<resTitle>ISO 19115 Topic Category</resTitle>
</thesaName>
</themeKeys>
<themeKeys>
<keyword>geology</keyword>
<keyword>geologic map</keyword>
<keyword>data</keyword>
<keyword>1:100000</keyword>
</themeKeys>
<searchKeys>
<keyword>geology</keyword>
<keyword>geologic map</keyword>
<keyword>data</keyword>
<keyword>1:100000</keyword>
<keyword>Cheyenne</keyword>
<keyword>Wyoming</keyword>
</searchKeys>
<resConst>
<Consts>
<useLimit>USE CONSTRAINTS: Users of these datasets are cautioned against using the data at scales different from those at which the maps were compiled. Using these data at a larger scale will not provide greater accuracy and is, in fact, a misuse of the data. --- The Wyoming State Geological Survey (WSGS) and State of Wyoming make no representation or warranty, expressed or implied, regarding the use, accuracy, or completeness of the data presented herein, or from a map printed from these data. The act of distribution shall not constitute such a warranty. The WSGS does not guarantee the digital data or any map printed from the data to be free of errors or inaccuracies. --- The WSGS and State of Wyoming disclaim any responsibility or liability for interpretations made from these digital data or from any map printed from these digital data, and for any decisions based on the digital data or printed maps. The WSGS and State of Wyoming retain and do not waive sovereign immunity. --- We request that credit be expressly given to the “Wyoming State Geological Survey” when citing information from this publication.</useLimit>
</Consts>
</resConst>
<resConst>
<LegConsts>
<useLimit>USE CONSTRAINTS: Users of these datasets are cautioned against using the data at scales different from those at which the maps were compiled. Using these data at a larger scale will not provide greater accuracy and is, in fact, a misuse of the data. --- The Wyoming State Geological Survey (WSGS) and State of Wyoming make no representation or warranty, expressed or implied, regarding the use, accuracy, or completeness of the data presented herein, or from a map printed from these data. The act of distribution shall not constitute such a warranty. The WSGS does not guarantee the digital data or any map printed from the data to be free of errors or inaccuracies. --- The WSGS and State of Wyoming disclaim any responsibility or liability for interpretations made from these digital data or from any map printed from these digital data, and for any decisions based on the digital data or printed maps. The WSGS and State of Wyoming retain and do not waive sovereign immunity. --- We request that credit be expressly given to the “Wyoming State Geological Survey” when citing information from this publication.</useLimit>
</LegConsts>
</resConst>
<aggrInfo>
<aggrDSName>
<resTitle>Geologic map of the Cheyenne 30’ x 60’ quadrangle, southeastern Wyoming, western Nebraska, and northern Colorado</resTitle>
<date>
<pubDate>1995-01-01</pubDate>
</date>
<citRespParty>
<rpOrgName>Alan J. Ver Ploeg</rpOrgName>
<role>
<RoleCd value="006">
</RoleCd>
</role>
</citRespParty>
<citRespParty>
<rpOrgName>Wyoming State Geological Survey</rpOrgName>
<rpCntInfo>
<cntAddress>
<delPoint>Laramie, WY</delPoint>
</cntAddress>
</rpCntInfo>
<role>
<RoleCd value="010">
</RoleCd>
</role>
</citRespParty>
<presForm>
<PresFormCd value="006">
</PresFormCd>
</presForm>
<presForm>
<fgdcGeoform>map</fgdcGeoform>
</presForm>
<datasetSeries>
<seriesName>Map Series</seriesName>
<issId>46</issId>
</datasetSeries>
</aggrDSName>
<assocType>
<AscTypeCd value="002">
</AscTypeCd>
</assocType>
</aggrInfo>
<spatRpType>
<SpatRepTypCd value="001">
</SpatRepTypCd>
</spatRpType>
<tpCat>
<TopicCatCd value="008">
</TopicCatCd>
</tpCat>
<dataExt>
<geoEle>
<GeoBndBox>
<exTypeCode>true</exTypeCode>
<westBL>-105.0009</westBL>
<eastBL>-103.9928</eastBL>
<northBL>41.5043</northBL>
<southBL>40.9936</southBL>
</GeoBndBox>
</geoEle>
</dataExt>
<dataExt>
<exDesc>publication date</exDesc>
<tempEle>
<TempExtent>
<exTemp>
<TM_Instant>
<tmPosition>2025-01-01</tmPosition>
</TM_Instant>
</exTemp>
</TempExtent>
</tempEle>
</dataExt>
<suppInfo>Cheyenne_100k_BR_GeMS 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.</suppInfo>
</dataIdInfo>
<dqInfo>
<dqScope>
<scpLvl>
<ScopeCd value="005">
</ScopeCd>
</scpLvl>
</dqScope>
<report type="DQQuanAttAcc">
<measDesc>Confidence that a feature exists and confidence that a feature is correctly identified are described in per-feature attributes ExistenceConfidence and IdentityConfidence.
Confidence that a feature exists and confidence that a feature is correctly identified are described in per-feature attributes ExistenceConfidence and IdentityConfidence.</measDesc>
</report>
<report type="DQConcConsis">
<measDesc>Map elements and topology were checked if needed.</measDesc>
</report>
<report type="DQCompOm">
<measDesc>Dataset is considered complete for the information presented.</measDesc>
</report>
<report dimension="horizontal" type="DQAbsExtPosAcc">
<measDesc>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.
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.</measDesc>
</report>
<dataLineage>
<prcStep>
<stepDesc>In a GIS, digital datasets, nonspatial tables, and metadata were created and attributed in UTM Zone 13N NAD27, and reviewed to the USGS GeMS level 3 digital map standard.</stepDesc>
<stepDateTm>2025-01-01</stepDateTm>
</prcStep>
</dataLineage>
</dqInfo>
<spatRepInfo>
<VectSpatRep>
<geometObjs>
<geoObjTyp>
<GeoObjTypCd value="001">
</GeoObjTypCd>
</geoObjTyp>
<geoObjCnt>11</geoObjCnt>
</geometObjs>
<geometObjs>
<geoObjTyp>
<GeoObjTypCd value="002">
</GeoObjTypCd>
</geoObjTyp>
<geoObjCnt>1694</geoObjCnt>
</geometObjs>
<geometObjs>
<geoObjTyp>
<GeoObjTypCd value="002">
</GeoObjTypCd>
</geoObjTyp>
<geoObjCnt>2</geoObjCnt>
</geometObjs>
<geometObjs>
<geoObjTyp>
<GeoObjTypCd value="004">
</GeoObjTypCd>
</geoObjTyp>
<geoObjCnt>4</geoObjCnt>
</geometObjs>
<geometObjs>
<geoObjTyp>
<GeoObjTypCd value="001">
</GeoObjTypCd>
</geoObjTyp>
<geoObjCnt>589</geoObjCnt>
</geometObjs>
</VectSpatRep>
</spatRepInfo>
<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>Qt</edomv>
<edomvd>Terrace deposits</edomvd>
<edomvds>T | L</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qa</edomv>
<edomvd>Alluvial deposits</edomvd>
<edomvds>T | L</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ta</edomv>
<edomvd>ARIKAREE FORMATION (LOWER MIOCENE AND UPPER OLIGOCENE)</edomvd>
<edomvds>T | L</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qot</edomv>
<edomvd>Older terrace deposits (Pleistocene)</edomvd>
<edomvds>T | R</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Twr</edomv>
<edomvd>WHITE RIVER FORMATION (OLIGOCENE)</edomvd>
<edomvds>T | L</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qac</edomv>
<edomvd>Mixed alluvium and colluvium</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qsl</edomv>
<edomvd>Windblown sand and loess</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>To</edomv>
<edomvd>OGALLALA FORMATION (UPPER AND MIDDLE MIOCENE)</edomvd>
<edomvds>T | L</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qof</edomv>
<edomvd>Older alluvial fan deposits (Pleistocene)</edomvd>
<edomvds>T | R</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>DMUHeading1</edomv>
<edomvd>Paragraph style for first order heading. Times New Roman, Bold, 12 pt, 12 pt leading, all caps, centered.</edomvd>
<edomvds>U.S. Geological Survey National Cooperative Geologic Mapping Program, 2020, GeMS (Geologic Map Schema)—A standard format for the digital publication of geologic maps: U.S. Geological Survey Techniques and Methods, book 11, chap. B10, 74 p., https://doi.org//10.3133/tm11B10.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DMUHeading2</edomv>
<edomvd>Paragraph style for second order heading. Times New Roman, Bold, 10 pt, 12 pt leading, all caps, centered, 12 pt space before.</edomvd>
<edomvds>U.S. Geological Survey National Cooperative Geologic Mapping Program, 2020, GeMS (Geologic Map Schema)—A standard format for the digital publication of geologic maps: U.S. Geological Survey Techniques and Methods, book 11, chap. B10, 74 p., https://doi.org//10.3133/tm11B10.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DMUUnit1</edomv>
<edomvd>Paragraph style for formatted description of first-rank map unit. 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>U.S. Geological Survey National Cooperative Geologic Mapping Program, 2020, GeMS (Geologic Map Schema)—A standard format for the digital publication of geologic maps: U.S. Geological Survey Techniques and Methods, book 11, chap. B10, 74 p., https://doi.org//10.3133/tm11B10.</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>DAS01 | DAS11</edomv>
<edomvd>T | R</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS01 | DAS09</edomv>
<edomvd>T | L</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS01</edomv>
<edomvd>This study.</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>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>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>
</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>
</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>GeMS</edomv>
<edomvd>U.S. Geological Survey National Cooperative Geologic Mapping Program, 2020, GeMS (Geologic Map Schema)—A standard format for the digital publication of geologic maps: U.S. Geological Survey Techniques and Methods, book 11, chap. B10, 74 p., https://doi.org//10.3133/tm11B10.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>FGDC-STD-013-2006</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>AGI Glossary of Geology</edomv>
<edomvd>Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2005, Glossary of geology (5th ed.): Alexandria, Va., American Geological Institute, 779 p.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS01</edomv>
<edomvd>This study.</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>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>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>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>Eolian sediment</edomv>
<edomvd>Silt- and sand-sized sediment, deposited by wind.</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>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>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>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>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>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>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>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>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>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>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>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>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>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>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>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>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>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>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>Loess</edomv>
<edomvd>Silty sediment, deposited by wind, commonly near glacial margin.</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>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>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>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>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>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>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>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>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>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>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>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>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>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>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>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>Unmapped area</edomv>
<edomvd>Unmapped area</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>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 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>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>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>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>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>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>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>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>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>"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>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>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>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>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>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>Rock</edomv>
<edomvd>Various rock types, not differentiated.</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>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>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>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>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>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>Rock and sediment</edomv>
<edomvd>Various rocks and sediment, not differentiated.</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>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>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>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>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>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>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>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>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>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>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>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>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>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>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>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>Chert</edomv>
<edomvd>Sedimentary rock, composed chiefly of microcrystalline or cryptocrystalline quartz.</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>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>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>Mostly carbonate rock</edomv>
<edomvd>Mostly carbonate rock, interbedded with other sedimentary rock types.</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>Other materials</edomv>
<edomvd>Other materials</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>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>
<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>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>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>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>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>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>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>Limestone</edomv>
<edomvd>Carbonate sedimentary rock, consisting chiefly of calcite.</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>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>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>
</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>MiscellaneousMapInformation</enttypl>
<enttypd>Properties of the map report as a whole. May include title, authorship, scale, geologic mapping credit, editing credit, cartography credit, date of approval, local magnetic declination, publication series and number, and base map information.</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>MapProperty</attrlabl>
<attrdef>Name of map property. Examples include "Scale", "Authors and affiliations", "Magnetic declination".</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<udom>Unrepresentable domain. Free text.</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>MapPropertyValue</attrlabl>
<attrdef>Value of map property. Examples = "1:24,000", "G.S. Smith1 and J. Doe2 1-Division of Geology, Some State, 2-Big University", "16.5 degrees"</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<udom>Unrepresentable domain. Free text.</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>MiscellaneousMapInformation_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>DataSourcePolys</enttypl>
<enttypd>Polygons that delineate data sources for all parts of the map. 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>DataSourceID</attrlabl>
<attrdef>Source of data; foreign key to table DataSources.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<edom>
<edomv>DAS03</edomv>
<edomvd>Bjorkland, L.J., 1959, Geology and ground water resources of the upper Lodgepole Creek drainage basin, Wyoming: U.S. Geological Survey Water-Supply Paper 1483, 40 p., plate 1, scale 1:126,720.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS07</edomv>
<edomvd>Cooley, M.E., and Crist, M.A., 1994, Geohydrology of the High Plains aquifer system, Cheyenne urban area, Wyoming: U.S. Geological Survey Water Resources Investigations Report 92-4047, sheet 3, scale 1:15,840.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS09</edomv>
<edomvd>Lowry, M.E., and Crist, M.A., 1967, Geology and ground water resources of Laramie County, Wyoming: U.S. Geological Survey Water-Supply Paper 1834, 71 p., plate 1, scale 1:125,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS10</edomv>
<edomvd>Moore, F.E., 1959, The geomorphic evolution of the east flank of the Laramie Range [sic], Colorado and Wyoming: Laramie, University of Wyoming, unpublished Ph.D. dissertation, 123 p., plate 4, scale 1:63,360.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS05</edomv>
<edomvd>Cassiliano, Michael, 1980, Stratigraphy and vertebrate paleontology of the Horse Creek-Trail Creek area, Laramie County, Wyoming: University of Wyoming Contributions to Geology, v. 19, n. 1, p. 25-68, figure 3, scale 1:100,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS11</edomv>
<edomvd>Rapp, J.R., Warner, D.A., and Morgan, A.M., 1953, Geology and water resources of the Egbert-Pine Bluffs-Carpenter area, Laramie County, Wyoming: U.S. Geological Survey Water-Supply Paper 1140, 67 p., plate 1, scale 1:90,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS12</edomv>
<edomvd>State of Wyoming, 1987, Site proposal —superconducting super collider (SSC) U.S. Department of Energy-Geology and tunneling: State of Wyoming, v. 3, 57 p., figure 3.2.1-1a, scale 1:24,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS08</edomv>
<edomvd>Kirkham, R.M., and Wold, J.W., 1986, Water resources of upper Crow Creek, Colorado: Colorado Geological Survey Special Publication 29, 102 p., plate 1, scale 1:100,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS06</edomv>
<edomvd>Cooley, M.E., 1991, Quaternary geology of the northern Great Plains—The Cheyenne tableland, in Morrison, R.B., editor, Quaternary nonglacial geology, conterminous U.S.: Geological Society of America, The Geology of North America, D.N.A.G. v. K-2, p. 453-455, figure 10, scale 1:459,360.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS02</edomv>
<edomvd>Bjorkland, L.J., 1957, Geology and ground water resources of the lower Lodgepole Creek drainage basin, Nebraska: U.S. Geological Survey Water-Supply Paper 1410, 76 p., plate 1, scale 1:125,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS04</edomv>
<edomvd>Burchett, R.R., 1986, Geologic bedrock map of Nebraska: Nebraska Geological Survey, 1 plate, scale 1:1,000,000.</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>DataSourcePolys_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>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>
</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>contact</edomv>
<edomvd>A plane or irregular surface between two types or ages of rock; examples are faults, intrusive borders, bedding planes separating distinct strata, and unconformities.</edomvd>
<edomvds>Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2005, Glossary of geology (5th ed.): Alexandria, Va., American Geological Institute, 779 p.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>map boundary</edomv>
<edomvd>Line defining a spatial border around the mapped area.</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
</attr>
<attr>
<attrlabl>IsConcealed</attrlabl>
<attrdef>Flag for contacts and faults covered by overlying map unit.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>LocationConfidenceMeters</attrlabl>
<attrdef>Estimated half-width in meters of positional uncertainty envelope; position is relative to other features in database.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<udom>Positive real number. Value of -9, -99, or -999 indicates value is unknown.</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>ExistenceConfidence</attrlabl>
<attrdef>Confidence that feature exists.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<edom>
<edomv>certain</edomv>
<edomvd>Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation.</edomvd>
<edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
</edom>
</attrdomv>
</attr>
<attr>
<attrlabl>IdentityConfidence</attrlabl>
<attrdef>Confidence that feature is correctly identified.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<edom>
<edomv>certain</edomv>
<edomvd>Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation.</edomvd>
<edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
</edom>
</attrdomv>
</attr>
<attr>
<attrlabl>Label</attrlabl>
<attrdef>Plain-text equivalent of the desired annotation for a feature: for example "14 Ma", or "^c" which (when used with the FGDC GeoAge font) results in the geologic map-unit label TRc (with TR run together to make the Triassic symbol).</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>Symbol</attrlabl>
<attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>DataSourceID</attrlabl>
<attrdef>Source of data; foreign key to table DataSources.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<edom>
<edomv>DAS01</edomv>
<edomvd>This study.</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>
</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>anticline</edomv>
<edomvd>A fold, generally convex upward, whose core contains the stratigraphically older rocks.</edomvd>
<edomvds>Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., eds., 2005, Glossary of geology (5th ed.): Alexandria, Va., American Geological Institute, 779 p.</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>DAS01 | DAS09</edomv>
<edomvd>T | L</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS01</edomv>
<edomvd>This study.</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>GeologicLines_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>CartographicPoints</enttypl>
<enttypd>Points that represent independently placed line symbols, such as fault and fold decorations.</enttypd>
<enttypds>Wyoming State Geological Survey</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>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>line decoration</edomv>
<edomvd>Locations where line symbols (e.g., ball and bar, question mark) are independently placed on the map for better display.</edomvd>
<edomvds>This study.</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>Rotation</attrlabl>
<attrdef>Cartographic rotation, measured in degrees clockwise.</attrdef>
<attrdefs>Wyoming State Geological Survey</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>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>PlotAtScale</attrlabl>
<attrdef>At what scale (or larger) should this observation or analysis be plotted? At smaller scales, it should not be plotted. Useful to prevent crowding of display at small scales and to display progressively more data at larger and larger scales. Value is scale denominator.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<udom>Positive real number.</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>StationsID</attrlabl>
<attrdef>Foreign key to Stations point feature class.</attrdef>
<attrdefs>GeMS</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>Twr</edomv>
<edomvd>WHITE RIVER FORMATION (OLIGOCENE)</edomvd>
<edomvds>T | L</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qt</edomv>
<edomvd>Terrace deposits</edomvd>
<edomvds>T | L</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>To</edomv>
<edomvd>OGALLALA FORMATION (UPPER AND MIDDLE MIOCENE)</edomvd>
<edomvds>T | L</edomvds>
</edom>
</attrdomv>
</attr>
<attr>
<attrlabl>LocationSourceID</attrlabl>
<attrdef>Source of location; foreign key to table DataSources.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<edom>
<edomv>DAS01</edomv>
<edomvd>This study.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
</attr>
<attr>
<attrlabl>DataSourceID</attrlabl>
<attrdef>Source of data; foreign key to table DataSources.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<edom>
<edomv>DAS01</edomv>
<edomvd>This study.</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>CartographicPoints_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>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>MapUnit</attrlabl>
<attrdef>Short plain-text identifier of the map unit. Foreign key to DescriptionOfMapUnits table.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<edom>
<edomv>Qsl</edomv>
<edomvd>Windblown sand and loess</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qt</edomv>
<edomvd>Terrace deposits</edomvd>
<edomvds>T | L</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qa</edomv>
<edomvd>Alluvial deposits</edomvd>
<edomvds>T | L</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ta</edomv>
<edomvd>ARIKAREE FORMATION (LOWER MIOCENE AND UPPER OLIGOCENE)</edomvd>
<edomvds>T | L</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Twr</edomv>
<edomvd>WHITE RIVER FORMATION (OLIGOCENE)</edomvd>
<edomvds>T | L</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qot</edomv>
<edomvd>Older terrace deposits (Pleistocene)</edomvd>
<edomvds>T | R</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qac</edomv>
<edomvd>Mixed alluvium and colluvium</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>To</edomv>
<edomvd>OGALLALA FORMATION (UPPER AND MIDDLE MIOCENE)</edomvd>
<edomvds>T | L</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qof</edomv>
<edomvd>Older alluvial fan deposits (Pleistocene)</edomvd>
<edomvds>T | R</edomvds>
</edom>
</attrdomv>
</attr>
<attr>
<attrlabl>IdentityConfidence</attrlabl>
<attrdef>Confidence that feature is correctly identified.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<edom>
<edomv>certain</edomv>
<edomvd>Identity of a feature can be determined using relevant observations and scientific judgment; therefore, one can be reasonably confident in the credibility of this interpretation.</edomvd>
<edomvds>Federal Geographic Data Committee [prepared for the Federal Geographic Data Committee by the U.S. Geological Survey], 2006, FGDC Digital Cartographic Standard for Geologic Map Symbolization: Reston, Va., Federal Geographic Data Committee Document Number FGDC-STD-013-2006, 290 p., 2 plates.</edomvds>
</edom>
</attrdomv>
</attr>
<attr>
<attrlabl>Label</attrlabl>
<attrdef>Plain-text equivalent of the desired annotation for a feature: for example "14 Ma", or "^c" which (when used with the FGDC GeoAge font) results in the geologic map-unit label TRc (with TR run together to make the Triassic symbol).</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>Symbol</attrlabl>
<attrdef>Reference to a point marker, line symbol, or area-fill symbol that is used on the map graphic to denote the feature: perhaps a star for a K-Ar age locality, or a heavy black line for a fault.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>DataSourceID</attrlabl>
<attrdef>Source of data; foreign key to table DataSources.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<edom>
<edomv>DAS01</edomv>
<edomvd>This study.</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>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>
</detailed>
</eainfo>
</metadata>
