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<otherCitDet>Suggested citation:
Stafford, J.E., Hoffman, C.F., Wittke, S.J., Webber, P.M., and Frost, B.R., 2021, Preliminary geologic map of the Rock River 30' x 60' quadrangle, Albany, Laramie, and Platte counties, Wyoming: Wyoming State Geological Survey Open File Report 2021-5, scale 1:100,000.</otherCitDet>
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<idAbs>&lt;div&gt;&lt;div style='line-height:19px;'&gt;&lt;div&gt;The bedrock geology was completed by the Wyoming State Geological Survey for the digital geologic map of the Rock River, Wyoming 1:100,000 quadrangle. The geologic data were developed to provide regional scale geologic mapping for city and county planning, industrial and mineral development, and general public use.&lt;/div&gt;&lt;div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;div&gt;&lt;br /&gt;&lt;/div&gt;&lt;div&gt;Stafford, J.E., Hoffman, C.F., Wittke, S.J., Webber, P.M., and Frost, B.R., 2021, Preliminary geologic map of the Rock River 30' x 60' quadrangle, Albany, Laramie, and Platte counties, Wyoming: Wyoming State Geological Survey Open File Report 2021-5, scale 1:100,000.&lt;/div&gt;&lt;div&gt;&lt;br /&gt;&lt;/div&gt;&lt;div&gt;&lt;a href='https://www.wsgs.wyo.gov/pubs-maps/publication-search.aspx?PubID=OFR-2021-5' target='_blank'&gt;View/Download Other Available Formats&lt;/a&gt;&lt;/div&gt;</idAbs>
<idPurp>The bedrock geology was completed by the Wyoming State Geological Survey for the digital geologic map of the Rock River, Wyoming 1:100,000 quadrangle, Open File Report 2021-5. The geologic data were developed to provide regional scale geologic mapping for city and county planning, industrial and mineral development, and general public use.Stafford, J.E., Hoffman, C.F., Wittke, S.J., Webber, P.M., and Frost, B.R., 2021, Preliminary geologic map of the Rock River 30' x 60' quadrangle, Albany, Laramie, and Platte counties, Wyoming: Wyoming State Geological Survey Open File Report 2021-5, scale 1:100,000.View/Download Other Available Formats</idPurp>
<idCredit>Stafford, J.E., Hoffman, C.F., Wittke, S.J., Webber, P.M., and Frost, B.R., 2021, Preliminary geologic map of the Rock River 30' x 60' quadrangle, Albany, Laramie, and Platte counties, Wyoming: Wyoming State Geological Survey Open File Report 2021-5, scale 1:100,000.</idCredit>
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<city>Laramie</city>
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<keyword>Laramie Mountains</keyword>
<keyword>Laramie Range</keyword>
<keyword>Iron Mountain</keyword>
<keyword>Richeau Hills</keyword>
<keyword>McGill Anticline</keyword>
<keyword>Laramie Anorthosite Complex</keyword>
<keyword>Wheatland fault system</keyword>
<keyword>Wheatland Reservoir</keyword>
<keyword>Elmers greenstone belt</keyword>
<keyword>Precambrian</keyword>
<keyword>Paleozoic</keyword>
<keyword>Mesozoic</keyword>
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<useLimit>&lt;div style='text-align:Left;'&gt;&lt;div&gt;&lt;div&gt;&lt;p&gt;&lt;span&gt;USE CONSTRAINTS: Users of these datasets are cautioned against using the data at scales different from those at which the maps were compiled. Using this 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.&lt;/span&gt;&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;</useLimit>
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<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 this 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 the 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 the 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 the 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>
<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>
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-Style file included to symbolize layers. RockRiver_100k_BR_OFR-2021-5 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>
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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>
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<edom>
<edomv>Wea</edomv>
<edomvd>Amphibolite; Elmers Rock greenstone belt</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Wk</edomv>
<edomvd>Microcline augen granite gneiss; Squaw Rock granite</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qot</edomv>
<edomvd>Old terrace</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Wefb</edomv>
<edomvd>Felsic biotite gneiss; Elmers Rock greenstone belt</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Trc</edomv>
<edomvd>Chugwater Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Wem</edomv>
<edomvd>Marble; Elmers Rock greenstone belt</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Yld</edomv>
<edomvd>Granite and composite dikes; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kle</edomv>
<edomvd>Lewis Shale</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ysct</edomv>
<edomvd>Strong Creek troctolite; Strong Creek complex; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kmt</edomv>
<edomvd>Mowry Shale, Muddy Sandstone, and Thermopolis Shale</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ypmu</edomv>
<edomvd>Poe Mountain anorthosite, undifferentiated; Poe Mountain anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Xkd</edomv>
<edomvd>Kennedy dike swarm</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ymrfm</edomv>
<edomvd>Fine-grained monzonite; Maloin Ranch pluton; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ymrpm</edomv>
<edomvd>Porphyritic monzonite; Maloin Ranch pluton; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ypm4</edomv>
<edomvd>Lower leucogabbroic layered zone; Poe Mountain anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Yau</edomv>
<edomvd>Anorthosite, undifferentiated; Snow Creek, Poe Mountain, and Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kf</edomv>
<edomvd>Frontier Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ymrms</edomv>
<edomvd>Monzosyenite; Maloin Ranch pluton; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ypmlt</edomv>
<edomvd>Leucotroctolite; Poe Mountain anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ysbfm</edomv>
<edomvd>Ferromonzonite; Sybille intrusion; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>PPc</edomv>
<edomvd>Casper Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ypm2</edomv>
<edomvd>Middle anorthositic layered zone; Poe Mountain anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Twr</edomv>
<edomvd>White River Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ysbms</edomv>
<edomvd>Monzosyenite; Sybille intrusion; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kmv</edomv>
<edomvd>Mesaverde Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Twdr</edomv>
<edomvd>Wind River Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qal</edomv>
<edomvd>Alluvium</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kcv</edomv>
<edomvd>Cloverly Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Jm</edomv>
<edomvd>Morrison Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Tmo</edomv>
<edomvd>Miocene and Oligocene rocks, undivided</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kn</edomv>
<edomvd>Niobrara Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Pge</edomv>
<edomvd>Goose Egg Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ysbpm</edomv>
<edomvd>Porphyritic monzonite; Sybille intrusion; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Yca2</edomv>
<edomvd>Middle anorthositic layered zone; Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ycacf</edomv>
<edomvd>Coyote Flats anorthosite; Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ta</edomv>
<edomvd>Arikaree Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kmb</edomv>
<edomvd>Medicine Bow Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ypm5</edomv>
<edomvd>Upper leucogabbroic layered zone; Poe Mountain anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ycau</edomv>
<edomvd>Chugwater anorthosite, undivided; Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>KJs</edomv>
<edomvd>Cloverly, Morrison, and Sundance formations, undivided</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Tha</edomv>
<edomvd>Hanna Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ypm1</edomv>
<edomvd>Lower anorthositic layered zone; Poe Mountain anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ycaf</edomv>
<edomvd>Fractured anorthosite; Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>TrPu</edomv>
<edomvd>Goose Egg and Chugwater formations, undivided</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Yrmu</edomv>
<edomvd>Red Mountain pluton, undifferentiated; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qof</edomv>
<edomvd>Old fan</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kp</edomv>
<edomvd>Pierre Shale</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ysna</edomv>
<edomvd>Snow Creek anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Weps</edomv>
<edomvd>Pelitic schist; Elmers Rock greenstone belt</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ycagl</edomv>
<edomvd>Lower leucogabbroic layered zone; Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Wlgr</edomv>
<edomvd>Granite and granite gneiss, undifferentiated</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qt</edomv>
<edomvd>Terrace deposits</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>To</edomv>
<edomvd>Ogallala Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Yscbg</edomv>
<edomvd>Buttes granite; Strong Creek complex; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Yscg</edomv>
<edomvd>Greaser intrusion; Strong Creek complex; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qc</edomv>
<edomvd>Colluvium</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ymrg</edomv>
<edomvd>Granite, Maloin Ranch pluton; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Yca3</edomv>
<edomvd>Upper anorthositic layered zone (King Mountain anorthosite); Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ypm3</edomv>
<edomvd>Upper anorthositic layered zone; Poe Mountain anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Js</edomv>
<edomvd>Sundance Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qsl</edomv>
<edomvd>Sand and loess</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ycagu</edomv>
<edomvd>Upper leucogabbroic layered zone; Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ycagm</edomv>
<edomvd>Middle leucogabbroic layered zone; Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ks</edomv>
<edomvd>Steele Shale</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Water</edomv>
<edomvd>Water</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ysmc</edomv>
<edomvd>Mule Creek granite; Sherman batholith</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ql</edomv>
<edomvd>Playa lake lacustrine deposits</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Yca1</edomv>
<edomvd>Lower anorthositic layered zone; Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</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>DMUHeading2</edomv>
<edomvd>Paragraph style for second order heading.</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>
<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>DMUUnit2</edomv>
<edomvd>Paragraph style for formatted description of second-rank map unit. Times New Roman, Regular, 10 pt, 12 pt leading, left justified, 66 pt left indent, –10 pt 1st line indent, 3 pt space before.</edomvd>
<edomvds>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</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>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>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>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>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>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>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>Water or ice</edomv>
<edomvd>Water or ice</edomvd>
<edomvds>GeMS</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Sedimentary rock</edomv>
<edomvd>Consolidated material (rock) composed of particles transported and deposited by gravity, air, water, or ice, or accumulated by other natural agents operating at Earths surface, such as chemical precipitation or secretion by organisms. Does not here include sedimentary material directly deposited as result of volcanic activity.</edomvd>
<edomvds>GeMS</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Eolian sediment</edomv>
<edomvd>Silt- and sand-sized sediment, deposited by wind.</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>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>DAS01</edomv>
<edomvd>This study.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<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>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>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>
</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>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>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>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>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>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>Eolian sediment</edomv>
<edomvd>Silt- and sand-sized sediment, deposited by wind.</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>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>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>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>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>Chert</edomv>
<edomvd>Sedimentary rock, composed chiefly of microcrystalline or cryptocrystalline quartz.</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>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>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>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>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>Slate and phyllite, of sedimentary-rock origin</edomv>
<edomvd>Fine-grained rock derived from preexisting sedimentary rocks and altered by essentially solid-state mineralogical, chemical, or structural changes, in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Includes phyllite and slate (compact, fine-grained rock that possesses strong cleavage and, hence, can be split into slabs and thin plates). Mostly formed from fine-grained material such as mudstone.</edomvd>
<edomvds>GeMS</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Air-fall tephra</edomv>
<edomvd>Fragments of volcanic rock and lava, of various sizes, carried into air by explosions and by hot gases in eruption columns or lava fountains; known as tephra. As tephra falls to ground, with increasing distance from volcano, average size of individual rock particles and thickness of resulting deposit decrease. Fine tephra deposited at some distance from volcano is known as volcanic ash.</edomvd>
<edomvds>GeMS</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>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>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>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>Limestone</edomv>
<edomvd>Carbonate sedimentary rock, consisting chiefly of calcite.</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>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>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>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>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>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>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>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>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>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>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>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>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>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>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>Schist and gneiss, of sedimentary-rock origin</edomv>
<edomvd>Foliated rock derived from preexisting sedimentary rocks by essentially solid-state mineralogical, chemical, or structural changes in response to marked changes in temperature, pressure, deformation, and (or) chemical environment, generally at depth in Earths crust. Includes schist (characterized by such strong foliation or alignment of minerals that it readily splits into flakes or slabs) and gneiss (characterized by alternating, irregular bands of different mineral composition). Mostly formed from fine-grained material such as mudstone.</edomvd>
<edomvds>GeMS</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>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>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>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>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>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>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>Igneous and metamorphic rock</edomv>
<edomvd>Consists of coarse-grained intrusive igneous rock and generally medium- to high-grade metamorphic rock.</edomvd>
<edomvds>GeMS</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Sedimentary material</edomv>
<edomvd>An aggregation of particles deposited by gravity, air, water, or ice, or as accumulated by other natural agents operating at Earths surface such as chemical precipitation or secretion by organisms. May include unconsolidated material (sediment) and (or) sedimentary rock. Does not include sedimentary material directly deposited as a result of volcanic activity.</edomvd>
<edomvds>GeMS</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Other materials</edomv>
<edomvd>Other materials</edomvd>
<edomvds>GeMS</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Unmapped area</edomv>
<edomvd>Unmapped area</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>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>Rock and sediment</edomv>
<edomvd>Various rocks and sediment, not differentiated.</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>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>Rock</edomv>
<edomvd>Various rock types, not differentiated.</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>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>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>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>Glacial till, mostly sandy</edomv>
<edomvd>Mostly unsorted and unstratified material, generally unconsolidated, deposited directly by and underneath or adjacent to glacier without subsequent reworking by meltwater. Consists of heterogeneous mixture of clay, silt, sand, gravel, and boulders, ranging widely in size and shape. Relatively sandy in texture.</edomvd>
<edomvds>GeMS</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Fine-grained, 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>Mostly carbonate rock</edomv>
<edomvd>Mostly carbonate rock, interbedded with other sedimentary rock types.</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>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>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>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>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>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>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>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>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>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>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>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>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>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>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>"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>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>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>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>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>Colluvium and other widespread mass-movement sediment</edomv>
<edomvd>Sediment formed by slow, relatively widespread, downslope transport of particles or clasts produced by weathering and breakdown of underlying rock, sediment, and (or) soil. Composed of poorly sorted and poorly stratified material that ranges in size from clay to boulders.</edomvd>
<edomvds>GeMS</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Sandstone 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>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>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>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>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>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>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>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>Coarse-grained intrusive igneous rock</edomv>
<edomvd>Rock that solidified from molten or partly molten material (magma) at some depth beneath Earths surface, thereby cooling slowly enough for mineral crystals to grow large enough to be visible to naked eye.</edomvd>
<edomvds>GeMS</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Meta-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>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>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>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>Loess</edomv>
<edomvd>Silty sediment, deposited by wind, commonly near glacial margin.</edomvd>
<edomvds>GeMS</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Water or ice</edomv>
<edomvd>Water or ice</edomvd>
<edomvds>GeMS</edomvds>
</edom>
</attrdomv>
</attr>
<attr>
<attrlabl>IndentedName</attrlabl>
<attrdef>Name with addition of leading spaces to help show rank within a hierarchical list.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>Definition</attrlabl>
<attrdef>Plain-language definition.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
</detailed>
<detailed>
<enttyp>
<enttypl>MapUnitPolys</enttypl>
<enttypd>Polygons that record distribution of map units (including water, snowfields, glaciers, and unmapped area) on the particular map horizon. In the original file geodatabase, this dataset is found within the GeologicMap feature dataset.</enttypd>
<enttypds>GeMS</enttypds>
</enttyp>
<attr>
<attrlabl>OBJECTID</attrlabl>
<attrdef>Internal feature number</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>Shape</attrlabl>
<attrdef>Internal geometry object</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>MapUnit</attrlabl>
<attrdef>Short plain-text identifier of the map unit. Foreign key to DescriptionOfMapUnits table.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<edom>
<edomv>Wea</edomv>
<edomvd>Amphibolite; Elmers Rock greenstone belt</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Wk</edomv>
<edomvd>Microcline augen granite gneiss; Squaw Rock granite</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qot</edomv>
<edomvd>Old terrace</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Wefb</edomv>
<edomvd>Felsic biotite gneiss; Elmers Rock greenstone belt</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Trc</edomv>
<edomvd>Chugwater Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Wem</edomv>
<edomvd>Marble; Elmers Rock greenstone belt</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Yld</edomv>
<edomvd>Granite and composite dikes; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kle</edomv>
<edomvd>Lewis Shale</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ysct</edomv>
<edomvd>Strong Creek troctolite; Strong Creek complex; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kmt</edomv>
<edomvd>Mowry Shale, Muddy Sandstone, and Thermopolis Shale</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ypmu</edomv>
<edomvd>Poe Mountain anorthosite, undifferentiated; Poe Mountain anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Xkd</edomv>
<edomvd>Kennedy dike swarm</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ymrfm</edomv>
<edomvd>Fine-grained monzonite; Maloin Ranch pluton; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ymrpm</edomv>
<edomvd>Porphyritic monzonite; Maloin Ranch pluton; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ypm4</edomv>
<edomvd>Lower leucogabbroic layered zone; Poe Mountain anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Yau</edomv>
<edomvd>Anorthosite, undifferentiated; Snow Creek, Poe Mountain, and Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kf</edomv>
<edomvd>Frontier Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ymrms</edomv>
<edomvd>Monzosyenite; Maloin Ranch pluton; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ypmlt</edomv>
<edomvd>Leucotroctolite; Poe Mountain anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ysbfm</edomv>
<edomvd>Ferromonzonite; Sybille intrusion; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>PPc</edomv>
<edomvd>Casper Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Pge</edomv>
<edomvd>Goose Egg Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ypm2</edomv>
<edomvd>Middle anorthositic layered zone; Poe Mountain anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Twr</edomv>
<edomvd>White River Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ysbms</edomv>
<edomvd>Monzosyenite; Sybille intrusion; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kmv</edomv>
<edomvd>Mesaverde Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qal</edomv>
<edomvd>Alluvium</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ycacf</edomv>
<edomvd>Coyote Flats anorthosite; Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Yca2</edomv>
<edomvd>Middle anorthositic layered zone; Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Twdr</edomv>
<edomvd>Wind River Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Tmo</edomv>
<edomvd>Miocene and Oligocene rocks, undivided</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kn</edomv>
<edomvd>Niobrara Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ysbpm</edomv>
<edomvd>Porphyritic monzonite; Sybille intrusion; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kcv</edomv>
<edomvd>Cloverly Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Jm</edomv>
<edomvd>Morrison Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ta</edomv>
<edomvd>Arikaree Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kmb</edomv>
<edomvd>Medicine Bow Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ycau</edomv>
<edomvd>Chugwater anorthosite, undivided; Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ypm5</edomv>
<edomvd>Upper leucogabbroic layered zone; Poe Mountain anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>KJs</edomv>
<edomvd>Cloverly, Morrison, and Sundance formations, undivided</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Tha</edomv>
<edomvd>Hanna Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ypm1</edomv>
<edomvd>Lower anorthositic layered zone; Poe Mountain anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ycaf</edomv>
<edomvd>Fractured anorthosite; Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>TrPu</edomv>
<edomvd>Goose Egg and Chugwater formations, undivided</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ysna</edomv>
<edomvd>Snow Creek anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kp</edomv>
<edomvd>Pierre Shale</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qof</edomv>
<edomvd>Old fan</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Weps</edomv>
<edomvd>Pelitic schist; Elmers Rock greenstone belt</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Yrmu</edomv>
<edomvd>Red Mountain pluton, undifferentiated; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ycagl</edomv>
<edomvd>Lower leucogabbroic layered zone; Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Wlgr</edomv>
<edomvd>Granite and granite gneiss, undifferentiated</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qt</edomv>
<edomvd>Terrace deposits</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>To</edomv>
<edomvd>Ogallala Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ycagm</edomv>
<edomvd>Middle leucogabbroic layered zone; Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Yscbg</edomv>
<edomvd>Buttes granite; Strong Creek complex; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qc</edomv>
<edomvd>Colluvium</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ymrg</edomv>
<edomvd>Granite, Maloin Ranch pluton; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Yca3</edomv>
<edomvd>Upper anorthositic layered zone (King Mountain anorthosite); Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Yscg</edomv>
<edomvd>Greaser intrusion; Strong Creek complex; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ypm3</edomv>
<edomvd>Upper anorthositic layered zone; Poe Mountain anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qsl</edomv>
<edomvd>Sand and loess</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ycagu</edomv>
<edomvd>Upper leucogabbroic layered zone; Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Js</edomv>
<edomvd>Sundance Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ks</edomv>
<edomvd>Steele Shale</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Water</edomv>
<edomvd>Water</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ysmc</edomv>
<edomvd>Mule Creek granite; Sherman batholith</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ql</edomv>
<edomvd>Playa lake lacustrine deposits</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Yca1</edomv>
<edomvd>Lower anorthositic layered zone; Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</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>
<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>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>map boundary</edomv>
<edomvd>Line defining a spatial border around the mapped area.</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<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>normal fault</edomv>
<edomvd>A fault in which the hanging wall has moved downward relative to the footwall. The angle of the fault is usually 45-90°, and in most cases close to 60°.</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>reverse fault</edomv>
<edomvd>A fault on which the hanging wall has moved upward relative to the footwall. The dip of the fault is usually greater than 45°.</edomvd>
<edomvds>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>fault</edomv>
<edomvd>A discrete surface or zone of discrete surfaces separating two rock masses across which one mass has slid past the other.</edomvd>
<edomvds>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>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>
<attr>
<attrlabl>Shape_Length</attrlabl>
<attrdef>Internal feature length, double</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
</detailed>
<detailed>
<enttyp>
<enttypl>GeologicLines</enttypl>
<enttypd>Lines that represent dikes, coal seams, ash beds, fold hinge-surface traces, isograds, and other linear features. All have these properties: (A) They do not participate in map-unit topology. (B) They correspond to features that exist within the Earth and may be concealed beneath younger, covering, material. (C) They are located with an accuracy that likely can be estimated. In the original file geodatabase, this dataset is found within the GeologicMap feature dataset.</enttypd>
<enttypds>GeMS</enttypds>
</enttyp>
<attr>
<attrlabl>OBJECTID</attrlabl>
<attrdef>Internal feature number</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>Shape</attrlabl>
<attrdef>Internal geometry object</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>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>syncline</edomv>
<edomvd>A fold of which the core contains the stratigraphically younger rocks; it is generally concave upward.</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>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</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>
<attr>
<attrlabl>Shape_Length</attrlabl>
<attrdef>Internal feature length, double</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
</detailed>
<detailed>
<enttyp>
<enttypl>GenericPoints</enttypl>
<enttypd>Miscellaneous points.</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>Trc</edomv>
<edomvd>Chugwater Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Wem</edomv>
<edomvd>Marble; Elmers Rock greenstone belt</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kmt</edomv>
<edomvd>Mowry Shale, Muddy Sandstone, and Thermopolis Shale</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Yau</edomv>
<edomvd>Anorthosite, undifferentiated; Snow Creek, Poe Mountain, and Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kf</edomv>
<edomvd>Frontier Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>PPc</edomv>
<edomvd>Casper Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Twr</edomv>
<edomvd>White River Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Pge</edomv>
<edomvd>Goose Egg Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Jm</edomv>
<edomvd>Morrison Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Kn</edomv>
<edomvd>Niobrara Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ta</edomv>
<edomvd>Arikaree Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ycau</edomv>
<edomvd>Chugwater anorthosite, undivided; Chugwater anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>TrPu</edomv>
<edomvd>Goose Egg and Chugwater formations, undivided</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ysna</edomv>
<edomvd>Snow Creek anorthosite; Laramie Anorthosite Complex</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Qt</edomv>
<edomvd>Terrace deposits</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Water</edomv>
<edomvd>Water</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Js</edomv>
<edomvd>Sundance Formation</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Ks</edomv>
<edomvd>Steele Shale</edomvd>
<edomvds>This study.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>Wefb</edomv>
<edomvd>Felsic biotite gneiss; Elmers Rock greenstone belt</edomvd>
<edomvds>This study.</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>GenericPoints_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>MapUnitPolysAnno</enttypl>
<enttypd>Annotation layer for MapUnitPolys.</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>FeatureID</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>ZOrder</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>AnnotationClassID</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>Element</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>SymbolID</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>Status</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>TextString</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>FontName</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>FontSize</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>Underline</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>VerticalAlignment</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>HorizontalAlignment</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>XOffset</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>YOffset</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>Angle</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>FontLeading</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>WordSpacing</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>CharacterWidth</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>CharacterSpacing</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>FlipAngle</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>Override</attrlabl>
<attrdef>BLOB field that stores feature-specific overrides to the cartographic representation rules.</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>FontStyle</attrlabl>
<attrdef>Value controls placement or representation of annotation</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Unrepresentable domain</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>DataSourceID</attrlabl>
<attrdef>Source of data; foreign key to table DataSources.</attrdef>
<attrdefs>GeMS</attrdefs>
<attrdomv>
<edom>
<edomv>DAS06</edomv>
<edomvd>Frost, B.R., 1993, Sybille Springs quadrangle field map (unpublished).</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS28</edomv>
<edomvd>McAndrews, Harry, 1965, Geologic map of the Bosler quadrangle, Albany County, Wyoming: U.S. Geological Survey Geologic Quadrangle GQ-509, scale 1:24,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS33</edomv>
<edomvd>McGrew, L.W., 1967, Geologic map of the Richeau Hills quadrangle, Platte County, Wyoming: U.S. Geological Survey Geologic Quadrangle GQ-625, scale 1:24,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS22</edomv>
<edomvd>Love, J.D., and Christiansen, A.C., comps, 1985, Geologic map of Wyoming: U.S. Geological Survey, 3 sheets, scale 1:500,000. (Re-released 2014, Wyoming State Geological Survey).</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS20</edomv>
<edomvd>Hyden, H.J., 1965, Geologic map of the Rock River quadrangle, Albany County, Wyoming: U.S. Geological Survey Geologic Quadrangle GQ-472, scale 1:24,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS34</edomv>
<edomvd>McGrew, L.W., 1967, Geologic map of the Squaw Rock quadrangle, Platte County, Wyoming: U.S. Geological Survey Geologic Quadrangle GQ-626, scale 1:24,000. Mitchell, J.N., 1993, Petrology and geochemistry of dioritic and gabbroic rocks in the Laramie Anorthosite Complex, Wyoming—Implications for the evolution of Proterozoic anorthosite: Laramie, University of Wyoming Ph.D. dissertation, 230 p.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS08</edomv>
<edomvd>Frost, B.R., Snyder, G.L., Lindsley, D.H., and Scoates, J.S., 1997, Laramie Anorthosite Complex field map, scale 1:100,000 (unpublished).</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS10</edomv>
<edomvd>Frost, B.R., Snyder, G.L., Lindsley, D.H., Scoates, J.S., and Anderson, I.C., in press b, Geologic map of the Poe Mountain quadrangle, Albany and Platte counties, Wyoming: Wyoming State Geological Survey Map Series 106, scale 1:24,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS31</edomv>
<edomvd>McGrew, L.W., 1967, Geologic map of the Natwick quadrangle, Platte County, Wyoming: U.S. Geological Survey Geologic Quadrangle GQ-624, scale 1:24,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS23</edomv>
<edomvd>Lindsley, D.H., Frost, B.R., Frost, C.D., and Scoates, J.S., 2010, Petrology, geochemistry, and structure of the Chugwater anorthosite, Laramie Anorthosite Complex, southeastern Wyoming: The Canadian Mineralogist, v. 48, p. 887–923.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS24</edomv>
<edomvd>Lowry, M.E., Crist, M.A., and Tilstra, J.R., 1967, Geology and ground-water resources of Laramie County, Wyoming: U.S. Geological Survey Water Supply Paper 1834, 71 p., 2 pls., scale 1:125,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS14</edomv>
<edomvd>Graff, P.J., Sears, J.W., Holden, G.S., and Hausel, W.D., 1982, Geology of the Elmers Rock greenstone belt Laramie Range, Wyoming: Wyoming State Geological Survey Report of Investigation 14, 24 p., 2 pls., scale 1:50,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS38</edomv>
<edomvd>Newhouse, W.H., and Hagner, A.F., 1957, Geologic map of anorthosite areas, southern part of Laramie Range, Wyoming: U.S. Geological Survey Miscellaneous Field Studies Map 119, scale 1:63,360.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS29</edomv>
<edomvd>McAndrews, Harry, 1965, Geologic map of the Cooper Lake North quadrangle, Albany County, Wyoming: U.S. Geological Survey Geologic Quadrangle GQ-430, scale 1:24,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS25</edomv>
<edomvd>Lowry, M.E., Rucker, S.J., and Wahl, K.L., 1973, Water resources of the Laramie, Shirley, and Hanna basins and adjacent areas, southeastern Wyoming: United States Geological Survey Hydrologic Atlas 471, scale 1:250,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS30</edomv>
<edomvd>McAndrews, Harry, 1966, Geologic map of the Lake Ione quadrangle, Albany County, Wyoming: U.S. Geological Survey Geologic Quadrangle GQ-508, scale 1:24,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS27</edomv>
<edomvd>McAndrews, Harry, 1964, Geologic map of the Cooper Lake South quadrangle, Albany County, Wyoming: U.S. Geological Survey Geologic Quadrangle GQ-391, scale 1:24,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS41</edomv>
<edomvd>Snyder, G.L., 1984, Preliminary geologic map of the central Laramie Mountains, Albany and Platte counties, Wyoming [Ayres Spring, Dodge Ranch, Bull Camp Peak, Moonshine Peak, Squaw Rock, Natwick, Bluegrass Wells, Guide Rock, Poe Mountain, Natwick SW, and Richeau Hills 7.5' quadrangles]: U.S. Geological Survey Open-File Report OF-84-358-A-L, scale 1:24,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS09</edomv>
<edomvd>Frost, B.R., Snyder, G.L., Lindsley, D.H., and Scoates, J.S., in press a, Geologic map of the Guide Rock quadrangle, Albany County, Wyoming: Wyoming State Geological Survey Map Series 105, scale 1:24,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS42</edomv>
<edomvd>Snyder, G.L., Budahn, J.R., Nealey, L.D., Bartel, A.J., and Ludwig, K.R., 1998, Geologic Map, Petrochemistry, and Geochronology of the Precambrian Rocks of the Bull Camp Peak Quadrangle, Albany County, Wyoming: U.S. Geological Survey Map I-2236, scale 1:24,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS13</edomv>
<edomvd>Frost, C.D., Frost, B.R., Lindsley, D.H., Chamberlain, K.R., Swapp, S.M., and Scoates, J.S., 2010, Geochemical and isotopic evolution of the anorthositic plutons of the Laramie Anorthosite Complex—Explanations for variations in silica activity and oxygen fugacity of massif anorthosites: The Canadian Mineralogist, v. 48, p. 925–946.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS17</edomv>
<edomvd>Haun, J.D., 1949, Geology of a portion of the east flank of the Laramie Range: Laramie, University of Wyoming M.A. thesis, 51 p., scale ~1:16,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS15</edomv>
<edomvd>Hammond, C.R., 1949, Geologic map and structure sections of the east flank of the Laramie Range in the vicinity of Iron Mountain, Wyoming: Laramie, University of Wyoming, M.A. thesis, 74 p., scale ~1:14,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS43</edomv>
<edomvd>Snyder, G.L., Peterman, Z.E., Love, J.D., and Langstaff, G.D., 1997, Geologic map and geochronology of the Precambrian and adjacent rocks of the Dodge Ranch–Ayres Spring area, Albany County, Wyoming: U.S. Geological Survey Map I-2235, scale 1:24,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS36</edomv>
<edomvd>Morgan, A.M., 1937, Geologic map of Laramie County, Wyoming—Showing well locations: Geological Survey of Wyoming [Wyoming State Geological Survey] Laramie County Map, scale 1:250,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS19</edomv>
<edomvd>Houlette, K.N., 1947, The Geology of McGill anticline, Albany County, Wyoming: Laramie, University of Wyoming M.A. thesis, 51 p., scale ~1:21,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS26</edomv>
<edomvd>McAndrews, Harry, 1964, Geologic map of the Big Judson quadrangle, Albany County, Wyoming: U.S. Geological Survey Geologic Quadrangle GQ-390, scale 1:24,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS37</edomv>
<edomvd>Morris, D.A., and Babcock, H.M., 1960, Geology and groundwater resources of Platte County, Wyoming: United States Geological Survey Water-Supply Paper 1490.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS04</edomv>
<edomvd>Frost, B.R., 1991, Sheep Rock quadrangle field map (unpublished).</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS05</edomv>
<edomvd>Frost, B.R., 1993, Baldy Mountain quadrangle field map (unpublished).</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS16</edomv>
<edomvd>Hallberg, L.L., and Case, J.C., 2005, Preliminary surficial geologic map of the Rock River 30' x 60' quadrangle, Albany, Platte, and Laramie counties, Wyoming: Wyoming State Geological Survey Open File Report 05-3, scale 1:100,000.</edomvd>
<edomvds>This report</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>DAS32</edomv>
<edomvd>McGrew, L.W., 1967, Geologic map of the Natwick SW quadrangle, Platte County, Wyoming: U.S. Geological Survey Geologic Quadrangle GQ-623, scale 1:24,000.</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>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>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>
</detailed>
</eainfo>
</metadata>
