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No fees are applicable for obtaining the data set.</resFees></distorOrdPrc><distorFormat><formatName>Vector Digital Data Set (Polygon)</formatName></distorFormat><distorTran><onLineSrc><linkage>https://doi.org/10.3133/sim3424</linkage></onLineSrc></distorTran></distributor><distTranOps><onLineSrc><linkage>https://pubs.er.usgs.gov/sim3424</linkage></onLineSrc><onLineSrc><linkage>https://doi.org/10.3133/sim3424</linkage></onLineSrc></distTranOps><distFormat><formatName>File Geodatabase Feature Class</formatName></distFormat></distInfo><dataIdInfo><idCitation><resTitle>Geology of the Hardeeville NW Quadrangle and Parts of the Brighton and Pineland Quadrangles, Jasper County, South Carolina</resTitle><date><pubDate>2019-02-11</pubDate></date><citRespParty><rpOrgName>Lucy E. Edwards</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>John P. McGeehin</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>William R. Doar III</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>U.S. Geological Survey</rpOrgName><rpCntInfo><cntAddress><delPoint>Reston, Virginia</delPoint></cntAddress></rpCntInfo><role><RoleCd value="010"/></role></citRespParty><citRespParty><rpOrgName>Christopher P. Garrity</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Arthur P. Schultz</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher E. Bernhardt</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher S. Swezey</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>E. 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Traditional geologic mapping in this area is difficult because of limited access, subdued topography, extensive swamps, and abundant vegetation.</idAbs><idPurp>The purpose of this information is to provide primary data for basic and applied earth-science investigations by producing geologic maps that contribute to a comprehensive nation-wide program of geologic mapping of bedrock and surface deposits.</idPurp><idCredit>Please acknowledge U.S. Geological Survey as the source of the data.</idCredit><idStatus><ProgCd value="001"/></idStatus><idPoC><rpIndName>Christopher Swezey</rpIndName><rpOrgName>U.S. Geological Survey, Northeast Region</rpOrgName><rpPosName>Research Geologist</rpPosName><rpCntInfo><cntPhone><voiceNum>703-648-6444</voiceNum><faxNum>703-648-6953</faxNum></cntPhone><cntAddress addressType="postal"><delPoint>Mail Stop 926A, 12201 Sunrise Valley Dr</delPoint><city>Reston</city><adminArea>VA</adminArea><postCode>20192</postCode><country>US</country><eMailAdd>cswezey@usgs.gov</eMailAdd></cntAddress></rpCntInfo><role><RoleCd value="007"/></role></idPoC><resMaint><maintFreq><MaintFreqCd value="011"/></maintFreq></resMaint><placeKeys><keyword>Pineville</keyword><keyword>Brighton</keyword><keyword>Jasper</keyword><keyword>United States</keyword><keyword>Hardeeville NW</keyword><keyword>South Carolina</keyword><thesaName><resTitle>Common geographic areas</resTitle></thesaName></placeKeys><themeKeys><keyword>geoscientificInformation</keyword><thesaName><resTitle>ISO 19115 Topic Category</resTitle></thesaName></themeKeys><themeKeys><keyword>Clay or mud</keyword><keyword>Sand</keyword><keyword>Gravel</keyword><keyword>Eolian material</keyword><keyword>Peat</keyword><keyword>Terrace</keyword><thesaName><resTitle>Lithologic classification of geologic map units</resTitle></thesaName></themeKeys><themeKeys><keyword>surficial geologic units</keyword><keyword>Quaternary</keyword><keyword>geologic time periods</keyword><keyword>Pliocene</keyword><keyword>Holocene</keyword><keyword>geologic maps</keyword><keyword>Miocene</keyword><keyword>geologic contacts</keyword><thesaName><resTitle>USGS Thesaurus</resTitle></thesaName></themeKeys><searchKeys><keyword>surficial geologic units</keyword><keyword>Quaternary</keyword><keyword>geologic time periods</keyword><keyword>Clay or mud</keyword><keyword>Sand</keyword><keyword>Pliocene</keyword><keyword>Gravel</keyword><keyword>Pineville</keyword><keyword>Brighton</keyword><keyword>Holocene</keyword><keyword>Eolian material</keyword><keyword>geologic maps</keyword><keyword>geoscientificInformation</keyword><keyword>Jasper</keyword><keyword>United States</keyword><keyword>Hardeeville NW</keyword><keyword>Peat</keyword><keyword>Miocene</keyword><keyword>Terrace</keyword><keyword>geologic contacts</keyword><keyword>South Carolina</keyword></searchKeys><resConst><LegConsts><useLimit>Although all data and software released have been used by the USGS, no warranty, expressed or implied, is made by the USGS as to the accuracy of the data and related materials and (or) the functioning of the software.</useLimit><othConsts>None. Please see 'Distribution Info' for details.</othConsts></LegConsts></resConst><resConst><Consts><useLimit>Unless otherwise stated, all data, metadata and related materials are considered to satisfy the quality standards relative to the purpose for which the data were collected. Although these data and associated metadata have been reviewed for accuracy and completeness and approved for release by the U.S. Geological Survey (USGS), no warranty expressed or implied is made regarding the display or utility of the data on any other system or for general or scientific purposes, nor shall the act of distribution constitute any such warranty. Users of this geospatial data and geologic information derived there from should acknowledge the U.S. Geological Survey as the source of the data. Although software enables a user to display images at various scales, map data in this report should not be used at scales greater than 1:24,000.</useLimit></Consts></resConst><spatRpType><SpatRepTypCd value="001"/></spatRpType><dataLang><languageCode value="eng"/><countryCode value="USA"/></dataLang><tpCat><TopicCatCd value="008"/></tpCat><envirDesc>Environment as of Metadata Creation: Microsoft Windows 7 Version 6.1 (Build 7601) Service Pack 1; Esri ArcGIS 10.6 (Build 8321) Service Pack N/A (Build N/A)</envirDesc><dataExt><exDesc>publication date</exDesc><tempEle><TempExtent><exTemp><TM_Period><tmBegin>2009-12-01</tmBegin><tmEnd>2019-02-11</tmEnd></TM_Period></exTemp></TempExtent></tempEle><geoEle/></dataExt><dataExt><geoEle><GeoBndBox><westBL>-81.281904467</westBL><eastBL>-81.124573748</eastBL><southBL>32.374939849</southBL><northBL>32.56019807</northBL></GeoBndBox></geoEle></dataExt><suppInfo>This feature class contains geologic unit boundaries for the Hardeeville NW quadrangle and parts of the Brighton and Pineland quadrangles, Jasper County, South Carolina. Digital data were compiled from source data at a scale of 1:24,000 and are not intended to be used at a larger (greater detail) scale. The release of these data will allow the general public, academia, and earth science professional to view and evaluate geologic data at the 1:24,000 scale. It is hoped that the use of these data, either by themselves or in relation to other data, may lead to new interpretations of the geology of the mapped area.</suppInfo><dataExt><geoEle><GeoBndBox esriExtentType="search"><exTypeCode>1</exTypeCode><westBL>-81.281904</westBL><eastBL>-81.124574</eastBL><northBL>32.560198</northBL><southBL>32.374940</southBL></GeoBndBox></geoEle></dataExt></dataIdInfo><dqInfo><dqScope><scpLvl><ScopeCd value="005"/></scpLvl></dqScope><report type="DQTopConsis"><evalMethDesc>Topological accuracy was tested using topology validation tools. Specific errors that were checked included: Polygon overlaps and gaps, coincident contact lines and geologic unit borders, self overlapping lines and superfluous pseudo nodes. No duplicate features exist nor duplicate points in a data string. Intersecting lines are separated into individual line segments at the point of intersection. Feature classes in the geodatabase are topologically clean.</evalMethDesc></report><report type="DQConcConsis"><measDesc>Topological accuracy was tested using topology validation tools. Specific errors that were checked included: Polygon overlaps and gaps, coincident contact lines and geologic unit borders, self overlapping lines and superfluous pseudo nodes. No duplicate features exist nor duplicate points in a data string. Intersecting lines are separated into individual line segments at the point of intersection. Feature classes in the geodatabase are topologically clean.</measDesc></report><report type="DQCompOm"><measDesc>Data set complete. No data was intentionally omitted from the source map.</measDesc></report><report type="DQQuanAttAcc"><measDesc>Attribute accuracy was tested by manual comparison of the source with hard copy printouts and/or symbolized display of the digital geologic data on an interactive computer graphic system. In addition, attributes were compared to a master set of valid geologic unit attributes.</measDesc></report><report type="DQAbsExtPosAcc" dimension="horizontal"><measDesc>A formal accuracy assessment of the horizontal positional information in the data set has not been conducted.</measDesc></report><report type="DQAbsExtPosAcc" dimension="vertical"><measDesc>A formal accuracy assessment of the vertical positional information in the data set has either not been conducted, or is not applicable.</measDesc></report><dataLineage><prcStep><stepDesc>Swezey and Schultz dug pits into these features and noted sediment composition, noted changes in vegetation assemblages associated with some of the features, and collected sediment samples for OSL dating. Swezey and Schultz also compared the sediments found in their pits with USDA soil maps of Jasper County (Stuck, 1980). Swezey and Schultz also drilled cores in the field area in order to verify vertical stratigraphic contacts.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Crider took linework, smoothed it, and made sure that the linework was topologically clean and located properly. Swezey reviewed the resulting product, and made some modifications after checking against the field data obtained by Swezey and Schultz.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>LiDAR imagery of the field area was processed by Garrity, and field data were collected by Swezey and Schultz. Schultz placed mylar on top of the LiDAR plot, consulted with field data obtained by Swezey and Schultz, and traced over features of the hillshade.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Swezey and Schultz obtained LiDAR imagery of the Hardeeville NW quadrangle and the southern half of the Brighton and Pineland quadrangles.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Christopher Swezey and Arthur Schultz obtained previously published topographic maps and previously published geologic maps of the area (Doar, 2008, 2013a, 2013b).</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Swezey and Schultz field-checked the various geomorphological features that were visible in the LiDAR imagery, paying particular attention to boundaries of the geomorphologic features.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>The LiDAR was processed by Christopher Garrity. The LiDAR imagery revealed low-relief geomorphological features that were not apparent in the previously published maps.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Crider registered and rectified the mylar over the LiDAR hillshade in ArcGIS.Schultz directly digitized the linework onscreen, using a hillshade and slope DEM from the LiDAR DEM and the registered mylar.</stepDesc><stepDateTm date="unknown"/></prcStep></dataLineage></dqInfo><spatRepInfo><VectSpatRep><geometObjs><geoObjTyp><GeoObjTypCd value="002"/></geoObjTyp><geoObjCnt>695</geoObjCnt></geometObjs><topLvl><TopoLevCd value="001"/></topLvl></VectSpatRep></spatRepInfo><eainfo><detailed><enttyp><enttypl>Attribute Table</enttypl><enttypd>Table containing attribute information associated with the data set.</enttypd><enttypds>Producer defined</enttypds></enttyp><attr><attrlabl>OBJECTID</attrlabl><attrdef>Internal feature number.</attrdef><attrdefs>Esri</attrdefs><attrdomv><udom>Sequential unique whole numbers that are automatically generated.</udom></attrdomv></attr><attr><attrlabl>SHAPE</attrlabl><attrdef>Feature geometry.</attrdef><attrdefs>Esri</attrdefs><attrdomv><udom>Coordinates defining the features.</udom></attrdomv></attr><attr><attrlabl>MapUnit</attrlabl><attrdef>Short plain-text identifier of the map unit.</attrdef><attrdefs>Producer defined</attrdefs><attrdomv><edom><edomv>Qs2</edomv><edomvd>Sand (Quaternary) interpreted as fluvial bars, some of which have been reworked by eolian processes</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm2</edomv><edomvd>Sand and mud (Holocene) interpreted as levee deposits and crevasse splay deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Ngsm</edomv><edomvd>Gravel, sand, and mud (lower Pliocene?) interpreted as estuarine to marginal marine sediments and beach ridges</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm4</edomv><edomvd>Sand and mud (Quaternary) interpreted as extra-channel areas that are adjacent to but outside of a channel</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsmp3</edomv><edomvd>Sand, mud, and peat (Quaternary) interpreted as fluvial and swamp deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qs1</edomv><edomvd>Sand (Quaternary) interpreted as eolian dune deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qs3</edomv><edomvd>Sand terraces within the Savannah River flood plain (Quaternary) interpreted as fluvial terrace deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qgsm</edomv><edomvd>Gravel, sand, and mud (Pleistocene) interpreted as a fluvial deposit</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm3</edomv><edomvd>Sand and mud (Quaternary) interpreted as channel and point-bar deposits in relict meandering channels</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsmp2</edomv><edomvd>Sand, mud, and peat (Holocene) interpreted as alluvial or swamp deposits that accumulated in abandoned fluvial channels</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm1</edomv><edomvd>Sand and mud (Holocene) interpreted as fluvial channel point bar deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsmp4</edomv><edomvd>Sand, mud, and peat in fluvial channels (Quaternary) interpreted as fluvial and swamp deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm5</edomv><edomvd>Sand and mud (Pleistocene) interpreted as alluvial and fluvial sediments</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsmp1</edomv><edomvd>Sand, mud, and peat (Holocene) interpreted as interdune swamp deposits</edomvd><edomvds>Producer defined</edomvds></edom></attrdomv></attr><attr><attrlabl>SHAPE_Area</attrlabl><attrdef>Area of feature in internal units squared.</attrdef><attrdefs>ESRI</attrdefs><attrdomv><rdom><rdommin>16.7387930713137</rdommin><rdommax>33518221.7252577</rdommax></rdom><udom>Positive real numbers that are automatically generated.</udom></attrdomv></attr><attr><attrlabl>SHAPE_Length</attrlabl><attrdef>Length of feature in internal units.</attrdef><attrdefs>ESRI</attrdefs><attrdomv><rdom><rdommin>15.0048870911479</rdommin><rdommax>284191.070173028</rdommax><attrunit>meter</attrunit></rdom><udom>Positive real numbers that are automatically generated.</udom></attrdomv></attr><attr><attrlabl>mapDesc</attrlabl><attrdef>Defines and describes geologic map units in the feature class.</attrdef><attrdefs>Producer defined</attrdefs><attrdomv><udom>Defines and describes geologic map units in the feature class. 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value="eng"/><countryCode value="USA" Sync="TRUE"></countryCode></mdLang><mdChar><CharSetCd value="004"/></mdChar><mdHrLv><ScopeCd value="005"/></mdHrLv><mdContact><rpIndName>Christopher P Garrity</rpIndName><rpOrgName>U.S. Geological Survey, Midwest Region</rpOrgName><rpPosName>Cartographer</rpPosName><rpCntInfo><cntPhone><voiceNum>703-648-6426</voiceNum><faxNum>703-648-6419</faxNum></cntPhone><cntAddress addressType="postal"><delPoint>Mail Stop 956, 12201 Sunrise Valley Dr</delPoint><city>Reston</city><adminArea>VA</adminArea><postCode>20192</postCode><country>US</country><eMailAdd>cgarrity@usgs.gov</eMailAdd></cntAddress></rpCntInfo><role><RoleCd value="007"/></role></mdContact><mdDateSt>20190207</mdDateSt><mdStanName>ArcGIS Metadata</mdStanName><mdStanVer>1.0</mdStanVer><distInfo><distributor><distorCont><rpIndName>Christopher Swezey</rpIndName><rpOrgName>U.S. Geological Survey, Northeast Region</rpOrgName><rpPosName>Research Geologist</rpPosName><rpCntInfo><cntPhone><voiceNum>703-648-6444</voiceNum><faxNum>703-648-6953</faxNum></cntPhone><cntAddress addressType="postal"><delPoint>Mail Stop 926A, 12201 Sunrise Valley Dr</delPoint><city>Reston</city><adminArea>VA</adminArea><postCode>20192</postCode><country>US</country><eMailAdd>cswezey@usgs.gov</eMailAdd></cntAddress></rpCntInfo><role><RoleCd value="005"/></role></distorCont><distorOrdPrc><resFees>None. No fees are applicable for obtaining the data set.</resFees></distorOrdPrc><distorFormat><formatName>Digital Data</formatName></distorFormat><distorTran><onLineSrc><linkage>https://doi.org/10.3133/sim3424</linkage></onLineSrc></distorTran></distributor><distTranOps><onLineSrc><linkage>https://pubs.er.usgs.gov/sim3424</linkage></onLineSrc><onLineSrc><linkage>https://doi.org/10.3133/sim3424</linkage></onLineSrc></distTranOps><distFormat><formatName Sync="TRUE">File Geodatabase Feature Dataset</formatName></distFormat></distInfo><dataIdInfo><idCitation><resTitle>Geology of the Hardeeville NW Quadrangle and Parts of the Brighton and Pineland Quadrangles, Jasper County, South Carolina</resTitle><date><pubDate>2019-02-11</pubDate></date><citRespParty><rpOrgName>Lucy E. Edwards</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>John P. McGeehin</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>William R. Doar III</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>U.S. Geological Survey</rpOrgName><rpCntInfo><cntAddress><delPoint>Reston, Virginia</delPoint></cntAddress></rpCntInfo><role><RoleCd value="010"/></role></citRespParty><citRespParty><rpOrgName>Christopher P. Garrity</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Arthur P. Schultz</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher E. Bernhardt</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher S. Swezey</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>E. Allen Crider</rpOrgName><role><RoleCd value="006"/></role></citRespParty><presForm><fgdcGeoform>Vector Digital Data Set (Polygon)</fgdcGeoform><PresFormCd value="005" Sync="TRUE"></PresFormCd></presForm><datasetSeries><seriesName>U.S. Geological Survey Scientific Investigations Map</seriesName><issId>3424</issId></datasetSeries></idCitation><idAbs>This publication portrays the geology of the Hardeeville NW quadrangle and parts of the Brighton and Pineland quadrangles that are within Jasper County, South Carolina. This study area is located in the Atlantic Coastal Plain province, approximately 50 to 70 kilometers (km) inland from the coast. The data are compiled from geological field mapping, light detection and ranging (lidar) elevation data, cores, optically stimulated luminescence (OSL) ages, radiocarbon ages, and biostratigraphic interpretations. Most of the study area is occupied by the valley of the Savannah River, and exposures of geologic units are very limited. Traditional geologic mapping in this area is difficult because of limited access, subdued topography, extensive swamps, and abundant vegetation.</idAbs><idPurp>The purpose of this information is to provide primary data for basic and applied earth-science investigations by producing geologic maps that contribute to a comprehensive nation-wide program of geologic mapping of bedrock and surface deposits.</idPurp><idCredit>Please acknowledge U.S. Geological Survey as the source of the data.</idCredit><idStatus><ProgCd value="001"/></idStatus><idPoC><rpIndName>Christopher Swezey</rpIndName><rpOrgName>U.S. Geological Survey, Northeast Region</rpOrgName><rpPosName>Research Geologist</rpPosName><rpCntInfo><cntPhone><voiceNum>703-648-6444</voiceNum><faxNum>703-648-6953</faxNum></cntPhone><cntAddress addressType="postal"><delPoint>Mail Stop 926A, 12201 Sunrise Valley Dr</delPoint><city>Reston</city><adminArea>VA</adminArea><postCode>20192</postCode><country>US</country><eMailAdd>cswezey@usgs.gov</eMailAdd></cntAddress></rpCntInfo><role><RoleCd value="007"/></role></idPoC><resMaint><maintFreq><MaintFreqCd value="011"/></maintFreq></resMaint><placeKeys><keyword>Pineville</keyword><keyword>Brighton</keyword><keyword>Jasper</keyword><keyword>United States</keyword><keyword>Hardeeville NW</keyword><keyword>South Carolina</keyword><thesaName><resTitle>Common geographic areas</resTitle></thesaName></placeKeys><themeKeys><keyword>geoscientificInformation</keyword><thesaName><resTitle>ISO 19115 Topic Category</resTitle></thesaName></themeKeys><themeKeys><keyword>Clay or mud</keyword><keyword>Sand</keyword><keyword>Gravel</keyword><keyword>Eolian material</keyword><keyword>Peat</keyword><keyword>Terrace</keyword><thesaName><resTitle>Lithologic classification of geologic map units</resTitle></thesaName></themeKeys><themeKeys><keyword>surficial geologic units</keyword><keyword>Quaternary</keyword><keyword>geologic time periods</keyword><keyword>Pliocene</keyword><keyword>Holocene</keyword><keyword>geologic maps</keyword><keyword>Miocene</keyword><keyword>geologic contacts</keyword><thesaName><resTitle>USGS Thesaurus</resTitle></thesaName></themeKeys><searchKeys><keyword>surficial geologic units</keyword><keyword>Quaternary</keyword><keyword>geologic time periods</keyword><keyword>Clay or mud</keyword><keyword>Sand</keyword><keyword>Pliocene</keyword><keyword>Gravel</keyword><keyword>Pineville</keyword><keyword>Brighton</keyword><keyword>Holocene</keyword><keyword>Eolian material</keyword><keyword>geologic maps</keyword><keyword>geoscientificInformation</keyword><keyword>Jasper</keyword><keyword>United States</keyword><keyword>Hardeeville NW</keyword><keyword>Peat</keyword><keyword>Miocene</keyword><keyword>Terrace</keyword><keyword>geologic contacts</keyword><keyword>South Carolina</keyword></searchKeys><resConst><LegConsts><useLimit>Although all data and software released have been used by the USGS, no warranty, expressed or implied, is made by the USGS as to the accuracy of the data and related materials and (or) the functioning of the software.</useLimit><othConsts>None. Please see 'Distribution Info' for details.</othConsts></LegConsts></resConst><resConst><Consts><useLimit>Unless otherwise stated, all data, metadata and related materials are considered to satisfy the quality standards relative to the purpose for which the data were collected. Although these data and associated metadata have been reviewed for accuracy and completeness and approved for release by the U.S. Geological Survey (USGS), no warranty expressed or implied is made regarding the display or utility of the data on any other system or for general or scientific purposes, nor shall the act of distribution constitute any such warranty. Users of this geospatial data and geologic information derived there from should acknowledge the U.S. Geological Survey as the source of the data. Although software enables a user to display images at various scales, map data in this report should not be used at scales greater than 1:24,000.</useLimit></Consts></resConst><spatRpType><SpatRepTypCd value="001"/></spatRpType><dataLang><languageCode value="eng"/><countryCode value="USA" Sync="TRUE"></countryCode></dataLang><tpCat><TopicCatCd value="008"/></tpCat><envirDesc>Environment as of Metadata Creation: Microsoft Windows 7 Version 6.1 (Build 7601) Service Pack 1; Esri ArcGIS 10.6 (Build 8321) Service Pack N/A (Build N/A)</envirDesc><dataExt><exDesc>publication date</exDesc><tempEle><TempExtent><exTemp><TM_Period><tmBegin>2009-12-01</tmBegin><tmEnd>2019-02-11</tmEnd></TM_Period></exTemp></TempExtent></tempEle><geoEle/></dataExt><dataExt><geoEle><GeoBndBox><westBL>-81.2819</westBL><eastBL>-81.1246</eastBL><southBL>32.3749</southBL><northBL>32.5602</northBL></GeoBndBox></geoEle></dataExt><suppInfo>This feature class contains geologic unit boundaries for the Hardeeville NW quadrangle and parts of the Brighton and Pineland quadrangles, Jasper County, South Carolina. Digital data were compiled from source data at a scale of 1:24,000 and are not intended to be used at a larger (greater detail) scale. The release of these data will allow the general public, academia, and earth science professional to view and evaluate geologic data at the 1:24,000 scale. It is hoped that the use of these data, either by themselves or in relation to other data, may lead to new interpretations of the geology of the mapped area.</suppInfo><dataExt><geoEle><GeoBndBox esriExtentType="search"><exTypeCode Sync="TRUE">1</exTypeCode><westBL Sync="TRUE">-81.281904</westBL><eastBL Sync="TRUE">-81.124574</eastBL><northBL Sync="TRUE">32.560198</northBL><southBL Sync="TRUE">32.374940</southBL></GeoBndBox></geoEle></dataExt></dataIdInfo><dqInfo><dqScope><scpLvl><ScopeCd value="005"/></scpLvl></dqScope><report type="DQTopConsis"><evalMethDesc>Topological accuracy was tested using topology validation tools. Specific errors that were checked included: Polygon overlaps and gaps, coincident contact lines and geologic unit borders, self overlapping lines and superfluous pseudo nodes. No duplicate features exist nor duplicate points in a data string. Intersecting lines are separated into individual line segments at the point of intersection. Feature classes in the geodatabase are topologically clean.</evalMethDesc></report><report type="DQConcConsis"><measDesc>Topological accuracy was tested using topology validation tools. Specific errors that were checked included: Polygon overlaps and gaps, coincident contact lines and geologic unit borders, self overlapping lines and superfluous pseudo nodes. No duplicate features exist nor duplicate points in a data string. Intersecting lines are separated into individual line segments at the point of intersection. Feature classes in the geodatabase are topologically clean.</measDesc></report><report type="DQCompOm"><measDesc>Data set complete. No data was intentionally omitted from the source map.</measDesc></report><report type="DQQuanAttAcc"><measDesc>Attribute accuracy was tested by manual comparison of the source with hard copy printouts and/or symbolized display of the digital geologic data on an interactive computer graphic system. In addition, attributes were compared to a master set of valid geologic unit attributes.</measDesc></report><report type="DQAbsExtPosAcc" dimension="horizontal"><measDesc>A formal accuracy assessment of the horizontal positional information in the data set has not been conducted.</measDesc></report><report type="DQAbsExtPosAcc" dimension="vertical"><measDesc>A formal accuracy assessment of the vertical positional information in the data set has either not been conducted, or is not applicable.</measDesc></report><dataLineage><prcStep><stepDesc>Swezey and Schultz dug pits into these features and noted sediment composition, noted changes in vegetation assemblages associated with some of the features, and collected sediment samples for OSL dating. Swezey and Schultz also compared the sediments found in their pits with USDA soil maps of Jasper County (Stuck, 1980). Swezey and Schultz also drilled cores in the field area in order to verify vertical stratigraphic contacts.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Crider took linework, smoothed it, and made sure that the linework was topologically clean and located properly. Swezey reviewed the resulting product, and made some modifications after checking against the field data obtained by Swezey and Schultz.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>LiDAR imagery of the field area was processed by Garrity, and field data were collected by Swezey and Schultz. Schultz placed mylar on top of the LiDAR plot, consulted with field data obtained by Swezey and Schultz, and traced over features of the hillshade.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Swezey and Schultz obtained LiDAR imagery of the Hardeeville NW quadrangle and the southern half of the Brighton and Pineland quadrangles.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Christopher Swezey and Arthur Schultz obtained previously published topographic maps and previously published geologic maps of the area (Doar, 2008, 2013a, 2013b).</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Swezey and Schultz field-checked the various geomorphological features that were visible in the LiDAR imagery, paying particular attention to boundaries of the geomorphologic features.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>The LiDAR was processed by Christopher Garrity. The LiDAR imagery revealed low-relief geomorphological features that were not apparent in the previously published maps.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Crider registered and rectified the mylar over the LiDAR hillshade in ArcGIS.Schultz directly digitized the linework onscreen, using a hillshade and slope DEM from the LiDAR DEM and the registered mylar.</stepDesc><stepDateTm date="unknown"/></prcStep><dataSource><srcDesc>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, contacts and faults, or the additional supporting structural and cartographic information.</srcDesc><srcMedName><MedNameCd value="018"/></srcMedName><srcCitatn><resTitle>A revision of the lithostratigraphic units of the Coastal Plain of Georgia</resTitle><resAltTitle>Huddlestun, 1988</resAltTitle><date><pubDate>1988-01-01</pubDate></date><citRespParty><rpOrgName>Paul F. Huddlestun</rpOrgName><role><RoleCd value="006"/></role></citRespParty><presForm><fgdcGeoform>publication</fgdcGeoform></presForm><datasetSeries><seriesName>Georgia Geologic Bulletin</seriesName><issId>104</issId></datasetSeries><otherCitDet>Huddlestun, P.F., 1988, A revision of the lithostratigraphic units of the Coastal Plain of Georgiaâ€”The Miocene through Holocene: Georgia Geologic Survey Bulletin 104, 162 p. [Also available at https://epd.georgia.gov/sites/epd.georgia.gov/files/related_files/site_page/B-104.pdf.]</otherCitDet><citOnlineRes><linkage>https://epd.georgia.gov/sites/epd.georgia.gov/files/ related_files/site_page/B-104.pdf</linkage></citOnlineRes></srcCitatn><srcExt><exDesc>publication date</exDesc><tempEle><TempExtent><exTemp><TM_Instant><tmPosition>1988-01-01</tmPosition></TM_Instant></exTemp></TempExtent></tempEle></srcExt></dataSource><dataSource><srcDesc>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, contacts and faults, or the additional supporting structural and cartographic information.</srcDesc><srcMedName><MedNameCd value="018"/></srcMedName><srcScale><rfDenom>0</rfDenom></srcScale><srcCitatn><resTitle>Palynological studies reveal Holocene climate changes in a forested flood plain wetland, Savannah River valley, South Carolina (USA)</resTitle><resAltTitle>Bernhardt and others (2012)</resAltTitle><date><pubDate>2012-01-01</pubDate></date><citRespParty><rpOrgName>Arthur P. Schultz</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher Bernhardt</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher S. Swezey</rpOrgName><role><RoleCd value="006"/></role></citRespParty><presForm><fgdcGeoform>publication</fgdcGeoform></presForm><datasetSeries><seriesName>Geological Society of America Abstracts with Programs</seriesName><issId>v. 44, no. 7</issId></datasetSeries><otherCitDet>Bernhardt, C., Swezey, C.S., and Schultz, A.P., 2012, Palynological studies reveal Holocene climate changes in a forested flood plain wetland, Savannah River valley, South Carolina (USA) [abs.]: Geological Society of America Abstracts with Programs, v. 44, no. 7, p. 423. [Also available at https://gsa.confex.com/gsa/2012AM/webprogram/Paper211715.html.]</otherCitDet><citOnlineRes><linkage>https://gsa.confex.com/ gsa/2012AM/webprogram/Paper211715.html</linkage></citOnlineRes></srcCitatn><srcExt><exDesc>publication date</exDesc><tempEle><TempExtent><exTemp><TM_Instant><tmPosition>2012-01-01</tmPosition></TM_Instant></exTemp></TempExtent></tempEle></srcExt></dataSource><dataSource><srcDesc>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, contacts and faults, or the additional supporting structural and cartographic information.</srcDesc><srcMedName><MedNameCd value="018"/></srcMedName><srcCitatn><resTitle>Quaternary eolian dunes in the Savannah River Valley, Jasper County, South Carolina, USA</resTitle><resAltTitle>Swezey and others, 2013</resAltTitle><date><pubDate>2017-01-20</pubDate></date><citRespParty><rpOrgName>Cambridge University Press (CUP)</rpOrgName><rpCntInfo><cntAddress><delPoint>n/a</delPoint></cntAddress></rpCntInfo><role><RoleCd value="010"/></role></citRespParty><citRespParty><rpOrgName>Arthur P. Schultz</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>John P. McGeehin</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher P. Garrity</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Wilma AlemÃ¡n GonzÃ¡lez</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher S. Swezey</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher E. Bernhardt</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Shannon A. Mahan</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>William R. 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value="eng"/></mdLang><mdChar><CharSetCd value="004"/></mdChar><mdHrLv><ScopeCd value="005"/></mdHrLv><mdContact><rpIndName>Christopher P Garrity</rpIndName><rpOrgName>U.S. Geological Survey, Midwest Region</rpOrgName><rpPosName>Cartographer</rpPosName><rpCntInfo><cntPhone><voiceNum>703-648-6426</voiceNum><faxNum>703-648-6419</faxNum></cntPhone><cntAddress addressType="postal"><delPoint>Mail Stop 956, 12201 Sunrise Valley Dr</delPoint><city>Reston</city><adminArea>VA</adminArea><postCode>20192</postCode><country>US</country><eMailAdd>cgarrity@usgs.gov</eMailAdd></cntAddress></rpCntInfo><role><RoleCd value="007"/></role></mdContact><mdDateSt>20190207</mdDateSt><mdStanName>ArcGIS Metadata</mdStanName><mdStanVer>1.0</mdStanVer><distInfo><distributor><distorCont><rpIndName>Christopher Swezey</rpIndName><rpOrgName>U.S. Geological Survey, Northeast Region</rpOrgName><rpPosName>Research Geologist</rpPosName><rpCntInfo><cntPhone><voiceNum>703-648-6444</voiceNum><faxNum>703-648-6953</faxNum></cntPhone><cntAddress addressType="postal"><delPoint>Mail Stop 926A, 12201 Sunrise Valley Dr</delPoint><city>Reston</city><adminArea>VA</adminArea><postCode>20192</postCode><country>US</country><eMailAdd>cswezey@usgs.gov</eMailAdd></cntAddress></rpCntInfo><role><RoleCd value="005"/></role></distorCont><distorOrdPrc><resFees>None. No fees are applicable for obtaining the data set.</resFees></distorOrdPrc><distorFormat><formatName>Digital Data</formatName></distorFormat><distorTran><onLineSrc><linkage>https://doi.org/10.3133/sim3424</linkage></onLineSrc></distorTran></distributor><distTranOps><onLineSrc><linkage>https://pubs.er.usgs.gov/sim3424</linkage></onLineSrc><onLineSrc><linkage>https://doi.org/10.3133/sim3424</linkage></onLineSrc></distTranOps></distInfo><dataIdInfo><idCitation><resTitle>Geology of the Hardeeville NW Quadrangle and Parts of the Brighton and Pineland Quadrangles, Jasper County, South Carolina</resTitle><date><pubDate>2019-02-11</pubDate></date><citRespParty><rpOrgName>Lucy E. Edwards</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>John P. McGeehin</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>William R. Doar III</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>U.S. Geological Survey</rpOrgName><rpCntInfo><cntAddress><delPoint>Reston, Virginia</delPoint></cntAddress></rpCntInfo><role><RoleCd value="010"/></role></citRespParty><citRespParty><rpOrgName>Christopher P. Garrity</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Arthur P. Schultz</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher E. Bernhardt</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>E. Allen Crider</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher S. Swezey</rpOrgName><role><RoleCd value="006"/></role></citRespParty><presForm><fgdcGeoform>Vector Digital Data Set (Polygon)</fgdcGeoform></presForm><datasetSeries><seriesName>U.S. Geological Survey Scientific Investigations Map</seriesName><issId>3424</issId></datasetSeries></idCitation><idAbs>This publication portrays the geology of the Hardeeville NW quadrangle and parts of the Brighton and Pineland quadrangles that are within Jasper County, South Carolina. This study area is located in the Atlantic Coastal Plain province, approximately 50 to 70 kilometers (km) inland from the coast. The data are compiled from geological field mapping, light detection and ranging (lidar) elevation data, cores, optically stimulated luminescence (OSL) ages, radiocarbon ages, and biostratigraphic interpretations. Most of the study area is occupied by the valley of the Savannah River, and exposures of geologic units are very limited. Traditional geologic mapping in this area is difficult because of limited access, subdued topography, extensive swamps, and abundant vegetation.</idAbs><idPurp>The purpose of this information is to provide primary data for basic and applied earth-science investigations by producing geologic maps that contribute to a comprehensive nation-wide program of geologic mapping of bedrock and surface deposits.</idPurp><idCredit>Please acknowledge U.S. Geological Survey as the source of the data.</idCredit><idStatus><ProgCd value="001"/></idStatus><idPoC><rpIndName>Christopher Swezey</rpIndName><rpOrgName>U.S. Geological Survey, Northeast Region</rpOrgName><rpPosName>Research Geologist</rpPosName><rpCntInfo><cntPhone><voiceNum>703-648-6444</voiceNum><faxNum>703-648-6953</faxNum></cntPhone><cntAddress addressType="postal"><delPoint>Mail Stop 926A, 12201 Sunrise Valley Dr</delPoint><city>Reston</city><adminArea>VA</adminArea><postCode>20192</postCode><country>US</country><eMailAdd>cswezey@usgs.gov</eMailAdd></cntAddress></rpCntInfo><role><RoleCd value="007"/></role></idPoC><resMaint><maintFreq><MaintFreqCd value="011"/></maintFreq></resMaint><placeKeys><keyword>Pineville</keyword><keyword>Brighton</keyword><keyword>Jasper</keyword><keyword>United States</keyword><keyword>Hardeeville NW</keyword><keyword>South Carolina</keyword><thesaName><resTitle>Common geographic areas</resTitle></thesaName></placeKeys><themeKeys><keyword>geoscientificInformation</keyword><thesaName><resTitle>ISO 19115 Topic Category</resTitle></thesaName></themeKeys><themeKeys><keyword>geologic time periods</keyword><keyword>Pliocene</keyword><keyword>Holocene</keyword><keyword>geologic contacts</keyword><keyword>geologic maps</keyword><keyword>Quaternary</keyword><keyword>Miocene</keyword><keyword>surficial geologic units</keyword><thesaName><resTitle>USGS Thesaurus</resTitle></thesaName></themeKeys><themeKeys><keyword>Sand</keyword><keyword>Gravel</keyword><keyword>Eolian material</keyword><keyword>Clay or mud</keyword><keyword>Peat</keyword><keyword>Terrace</keyword><thesaName><resTitle>Lithologic classification of geologic map units</resTitle></thesaName></themeKeys><searchKeys><keyword>geologic time periods</keyword><keyword>Sand</keyword><keyword>Pliocene</keyword><keyword>Holocene</keyword><keyword>Pineville</keyword><keyword>Brighton</keyword><keyword>geologic contacts</keyword><keyword>Gravel</keyword><keyword>geologic maps</keyword><keyword>geoscientificInformation</keyword><keyword>Jasper</keyword><keyword>Eolian material</keyword><keyword>United States</keyword><keyword>Hardeeville NW</keyword><keyword>Clay or mud</keyword><keyword>Peat</keyword><keyword>Quaternary</keyword><keyword>Miocene</keyword><keyword>Terrace</keyword><keyword>South Carolina</keyword><keyword>surficial geologic units</keyword></searchKeys><resConst><LegConsts><useLimit>Although all data and software released have been used by the USGS, no warranty, expressed or implied, is made by the USGS as to the accuracy of the data and related materials and (or) the functioning of the software.</useLimit><othConsts>None. Please see 'Distribution Info' for details.</othConsts></LegConsts></resConst><resConst><Consts><useLimit>Unless otherwise stated, all data, metadata and related materials are considered to satisfy the quality standards relative to the purpose for which the data were collected. Although these data and associated metadata have been reviewed for accuracy and completeness and approved for release by the U.S. Geological Survey (USGS), no warranty expressed or implied is made regarding the display or utility of the data on any other system or for general or scientific purposes, nor shall the act of distribution constitute any such warranty. Users of this geospatial data and geologic information derived there from should acknowledge the U.S. Geological Survey as the source of the data. Although software enables a user to display images at various scales, map data in this report should not be used at scales greater than 1:24,000.</useLimit></Consts></resConst><spatRpType><SpatRepTypCd value="001"/></spatRpType><dataLang><languageCode value="eng"/></dataLang><tpCat><TopicCatCd value="008"/></tpCat><envirDesc>Environment as of Metadata Creation: Microsoft Windows 7 Version 6.1 (Build 7601) Service Pack 1; Esri ArcGIS 10.6 (Build 8321) Service Pack N/A (Build N/A)</envirDesc><dataExt><exDesc>publication date</exDesc><tempEle><TempExtent><exTemp><TM_Period><tmBegin>2009-12-01</tmBegin><tmEnd>2019-02-11</tmEnd></TM_Period></exTemp></TempExtent></tempEle></dataExt><dataExt><geoEle><GeoBndBox><westBL>-81.2791</westBL><eastBL>-81.1289</eastBL><southBL>32.4237</southBL><northBL>32.556</northBL></GeoBndBox></geoEle></dataExt><suppInfo>This feature class contains geologic unit boundaries for the Hardeeville NW quadrangle and parts of the Brighton and Pineland quadrangles, Jasper County, South Carolina. Digital data were compiled from source data at a scale of 1:24,000 and are not intended to be used at a larger (greater detail) scale. The release of these data will allow the general public, academia, and earth science professional to view and evaluate geologic data at the 1:24,000 scale. It is hoped that the use of these data, either by themselves or in relation to other data, may lead to new interpretations of the geology of the mapped area.</suppInfo></dataIdInfo><dqInfo><dqScope><scpLvl><ScopeCd value="005"/></scpLvl></dqScope><report type="DQTopConsis"><evalMethDesc>Topological accuracy was tested using topology validation tools. Specific errors that were checked included: Polygon overlaps and gaps, coincident contact lines and geologic unit borders, self overlapping lines and superfluous pseudo nodes. No duplicate features exist nor duplicate points in a data string. Intersecting lines are separated into individual line segments at the point of intersection. Feature classes in the geodatabase are topologically clean.</evalMethDesc></report><report type="DQConcConsis"><measDesc>Topological accuracy was tested using topology validation tools. Specific errors that were checked included: Polygon overlaps and gaps, coincident contact lines and geologic unit borders, self overlapping lines and superfluous pseudo nodes. No duplicate features exist nor duplicate points in a data string. Intersecting lines are separated into individual line segments at the point of intersection. Feature classes in the geodatabase are topologically clean.</measDesc></report><report type="DQCompOm"><measDesc>Data set complete. No data was intentionally omitted from the source map.</measDesc></report><report type="DQQuanAttAcc"><measDesc>Attribute accuracy was tested by manual comparison of the source with hard copy printouts and/or symbolized display of the digital geologic data on an interactive computer graphic system. In addition, attributes were compared to a master set of valid geologic unit attributes.</measDesc></report><report type="DQAbsExtPosAcc" dimension="horizontal"><measDesc>A formal accuracy assessment of the horizontal positional information in the data set has not been conducted.</measDesc></report><report type="DQAbsExtPosAcc" dimension="vertical"><measDesc>A formal accuracy assessment of the vertical positional information in the data set has either not been conducted, or is not applicable.</measDesc></report><dataLineage><prcStep><stepDesc>Christopher Swezey and Arthur Schultz obtained previously published topographic maps and previously published geologic maps of the area (Doar, 2008, 2013a, 2013b).</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Crider registered and rectified the mylar over the LiDAR hillshade in ArcGIS. Schultz directly digitized the linework onscreen, using a hillshade and slope DEM from the LiDAR DEM and the registered mylar.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Swezey and Schultz field-checked the various geomorphological features that were visible in the LiDAR imagery, paying particular attention to boundaries of the geomorphologic features.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Crider took linework, smoothed it, and made sure that the linework was topologically clean and located properly. Swezey reviewed the resulting product, and made some modifications after checking against the field data obtained by Swezey and Schultz.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Swezey and Schultz dug pits into these features and noted sediment composition, noted changes in vegetation assemblages associated with some of the features, and collected sediment samples for OSL dating. Swezey and Schultz also compared the sediments found in their pits with USDA soil maps of Jasper County (Stuck, 1980). Swezey and Schultz also drilled cores in the field area in order to verify vertical stratigraphic contacts.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Swezey and Schultz obtained LiDAR imagery of the Hardeeville NW quadrangle and the southern half of the Brighton and Pineland quadrangles.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>LiDAR imagery of the field area was processed by Garrity, and field data were collected by Swezey and Schultz. Schultz placed mylar on top of the LiDAR plot, consulted with field data obtained by Swezey and Schultz, and traced over features of the hillshade.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>The LiDAR was processed by Christopher Garrity. The LiDAR imagery revealed low-relief geomorphological features that were not apparent in the previously published maps.</stepDesc><stepDateTm date="unknown"/></prcStep><dataSource><srcDesc>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, contacts and faults, or the additional supporting structural and cartographic information.</srcDesc><srcMedName><MedNameCd value="018"/></srcMedName><srcCitatn><resTitle>Quaternary eolian dunes in the Savannah River Valley, Jasper County, South Carolina, USA</resTitle><resAltTitle>Swezey and others, 2013</resAltTitle><date><pubDate>2017-01-20</pubDate></date><citRespParty><rpOrgName>Wilma AlemÃ¡n GonzÃ¡lez</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Shannon A. Mahan</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Cambridge University Press (CUP)</rpOrgName><rpCntInfo><cntAddress><delPoint>n/a</delPoint></cntAddress></rpCntInfo><role><RoleCd value="010"/></role></citRespParty><citRespParty><rpOrgName>Christopher P. Garrity</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Arthur P. Schultz</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>William R. Doar</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>John P. McGeehin</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher S. Swezey</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher E. Bernhardt</rpOrgName><role><RoleCd value="006"/></role></citRespParty><presForm><fgdcGeoform>publication</fgdcGeoform></presForm><datasetSeries><seriesName>Quaternary Research</seriesName><issId>v. 80, no. 02</issId></datasetSeries><otherCitDet>Swezey, C.S., Schultz, A.P., AlemÃ¡n GonzÃ¡lez, W.B., Bernhardt, C.E., Doar, W.R., III, Garrity, C.P., Mahan, S.A., and McGeehin, J.P., 2013, Quaternary eolian dunes in the Savannah River Valley, Jasper County, South Carolina, USA: Quaternary Research, v. 80, no. 2, p. 250â€“264. [Also available at http://www.sciencedirect.com/science/article/pii/S0033589413000719.]</otherCitDet><citOnlineRes><linkage>http://dx.doi.org/10.1016/j.yqres.2013.06.007</linkage></citOnlineRes></srcCitatn><srcExt><exDesc>publication date</exDesc><tempEle><TempExtent><exTemp><TM_Instant><tmPosition>2017-01-01</tmPosition></TM_Instant></exTemp></TempExtent></tempEle></srcExt></dataSource></dataLineage></dqInfo><spatRepInfo><VectSpatRep><geometObjs><geoObjTyp><GeoObjTypCd value="004"/></geoObjTyp><geoObjCnt>20</geoObjCnt></geometObjs></VectSpatRep></spatRepInfo><eainfo><detailed><enttyp><enttypl>Attribute Table</enttypl><enttypd>Table containing attribute information associated with the data set.</enttypd><enttypds>Producer defined</enttypds></enttyp><attr><attrlabl>Latitude</attrlabl><attrdef>Latitude</attrdef></attr><attr><attrlabl>AgeDetermination</attrlabl><attrdef>Date the age of the sample was determined</attrdef></attr><attr><attrlabl>OSLSample</attrlabl><attrdef>OSL Sample ID</attrdef></attr><attr><attrlabl>OBJECTID</attrlabl><attrdef>Internal feature number.</attrdef><attrdefs>Esri</attrdefs><attrdomv><udom>Sequential unique whole numbers that are automatically generated.</udom></attrdomv></attr><attr><attrlabl>Longitude</attrlabl><attrdef>Longitude</attrdef></attr><attr><attrlabl>Shape</attrlabl><attrdef>Feature geometry.</attrdef><attrdefs>Esri</attrdefs><attrdomv><udom>Coordinates defining the features.</udom></attrdomv></attr><attr><attrlabl>AgeKa</attrlabl><attrdef>Age in thousands of years ago before present.</attrdef></attr></detailed><overview><eaover>The entity and attribute information provided here describes the tabular data associated with the data set. Please review the detailed descriptions that are provided (the individual attribute descriptions) for information on the values that appear as fields/table entries of the data set.</eaover><eadetcit>The entity and attribute information was generated by the individual and (or) agency identified as the originator of the data set. Please review the rest of the metadata record for additional details and information.</eadetcit></overview></eainfo></metadata>����`éÿÿsper County, South Carolina, USA</resTitle><resAltTitle>Swezey and others, 2013</resAltTitle><date><pubDate>2017-01-20</pubDate></date><citRespParty><rpOrgName>Cambridge University Press (CUP)</rpOrgName><rpCntInfo><cntAddress><delPoint>n/a</delPoint></cntAddress></rpCntInfo><role><RoleCd value="010"/></role></citRespParty><citRespParty><rpOrgName>Arthur P. Schultz</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>John P. McGeehin</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher P. Garrity</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Wilma AlemÃ¡n GonzÃ¡lez</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher S. Swezey</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher E. Bernhardt</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Shannon A. Mahan</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>William R. Doar</rpOrgName><role><RoleCd value="006"/></role></citRespParty><presForm><fgdcGeoform>publication</fgdcGeoform></presForm><datasetSeries><seriesName>Quaternary Research</seriesName><issId>v. 80, no. 02</issId></datasetSeries><otherCitDet>Swezey, C.S., Schultz, A.P., AlemÃ¡n GonzÃ¡lez, W.B., Bernhardt, C.E., Doar, W.R., III, Garrity, C.P., Mahan, S.A., and McGeehin, J.P., 2013, Quaternary eolian dunes in the Savannah River Valley, Jasper County, South Carolina, USA: Quaternary Research, v. 80, no. 2, p. 250â€“264. [Also available at http://www.sciencedirect.com/science/article/pii/S0033589413000719.]</otherCitDet><citOnlineRes><linkage>http://dx.doi.org/10.1016/j.yqres.2013.06.007</linkage></citOnlineRes></srcCitatn><srcExt><exDesc>publication date</exDesc><tempEle><TempExtent><exTemp><TM_Instant><tmPosition>2017-01-01</tmPosition></TM_Instant></exTemp></TempExtent></tempEle></srcExt></dataSource></dataLineage></dqInfo><spatRepInfo><VectSpatRep><geometObjs Name="GeochronPoints"><geoObjTyp><GeoObjTypCd value="004" Sync="TRUE"></GeoObjTypCd></geoObjTyp><geoObjCnt Sync="TRUE">20</geoObjCnt></geometObjs><topLvl><TopoLevCd value="001" Sync="TRUE"></TopoLevCd></topLvl></VectSpatRep></spatRepInfo><eainfo><detailed Name="GeochronPoints"><enttyp><enttypl>Attribute Table</enttypl><enttypd>Table containing attribute information associated with the data set.</enttypd><enttypds>Producer defined</enttypds><enttypt Sync="TRUE">Feature Class</enttypt><enttypc Sync="TRUE">20</enttypc></enttyp><attr><attrlabl Sync="TRUE">OBJECTID</attrlabl><attalias Sync="TRUE">OBJECTID</attalias><attrtype Sync="TRUE">OID</attrtype><attwidth Sync="TRUE">4</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale><attrdef Sync="TRUE">Internal feature number.</attrdef><attrdefs Sync="TRUE">Esri</attrdefs><attrdomv><udom Sync="TRUE">Sequential unique whole numbers that are automatically generated.</udom></attrdomv></attr><attr><attrlabl Sync="TRUE">Shape</attrlabl><attalias Sync="TRUE">Shape</attalias><attrtype Sync="TRUE">Geometry</attrtype><attwidth Sync="TRUE">0</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale><attrdef Sync="TRUE">Feature geometry.</attrdef><attrdefs Sync="TRUE">Esri</attrdefs><attrdomv><udom Sync="TRUE">Coordinates defining the features.</udom></attrdomv></attr><attr><attrlabl Sync="TRUE">OSLSample</attrlabl><attalias Sync="TRUE">OSLSample</attalias><attrtype Sync="TRUE">String</attrtype><attwidth Sync="TRUE">254</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr><attr><attrlabl Sync="TRUE">Latitude</attrlabl><attalias Sync="TRUE">Latitude</attalias><attrtype Sync="TRUE">Double</attrtype><attwidth Sync="TRUE">8</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr><attr><attrlabl Sync="TRUE">Longitude</attrlabl><attalias Sync="TRUE">Longitude</attalias><attrtype Sync="TRUE">Double</attrtype><attwidth Sync="TRUE">8</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr><attr><attrlabl Sync="TRUE">AgeDetermination</attrlabl><attalias Sync="TRUE">AgeDetermination</attalias><attrtype Sync="TRUE">Double</attrtype><attwidth Sync="TRUE">8</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr><attr><attrlabl Sync="TRUE">AgeKa</attrlabl><attalias Sync="TRUE">AgeKa</attalias><attrtype Sync="TRUE">String</attrtype><attwidth Sync="TRUE">254</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr></detailed><overview><eaover>The entity and attribute information provided here describes the tabular data associated with the data set. Please review the detailed descriptions that are provided (the individual attribute descriptions) for information on the values that appear as fields/table entries of the data set.</eaover><eadetcit>The entity and attribute information was generated by the individual and (or) agency identified as the originator of the data set. Please review the rest of the metadata record for additional details and information.</eadetcit></overview></eainfo><mdHrLvName Sync="TRUE">dataset</mdHrLvName><refSysInfo><RefSystem><refSysID><identCode code="4269" Sync="TRUE"></identCode><idCodeSpace Sync="TRUE">EPSG</idCodeSpace><idVersion Sync="TRUE">6.12(3.0.1)</idVersion></refSysID></RefSystem></refSysInfo><spdoinfo><ptvctinf><esriterm Name="GeochronPoints"><efeatyp Sync="TRUE">Simple</efeatyp><efeageom code="1" Sync="TRUE"></efeageom><esritopo Sync="TRUE">FALSE</esritopo><efeacnt Sync="TRUE">20</efeacnt><spindex Sync="TRUE">TRUE</spindex><linrefer Sync="TRUE">FALSE</linrefer></esriterm></ptvctinf></spdoinfo></metadata>����·Éÿÿsed of quartz (98 percent) and rock fragments (2 percent) that include mica and opaque minerals. The lower part of the unit is poorly to moderately sorted, whereas the upper part of the unit is moderately sorted to well sorted. Primary sedimentary structures are not apparent. Unit Qgsm forms an overall fining-upward sequence and is interpreted as a fluvial deposit. A terrace is formed on this unit in the southeasternmost part of the study area and appears to be greatly weathered. On the basis of elevation and geomorphological expression in the light detection and ranging (lidar) image (map B), the unit is thought to be older than terraces Qt1 through Qt5</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm5</edomv><edomvd>Sand and mud (Pleistocene)â€”0.3- to 9.1-m (1- to 30-ft)-thick, medium-light-gray (N6) to light-gray (N7) sand and muddy sand. Sand grains are fine to coarse grained and are composed predominantly of quartz. The unit is poorly to well sorted. Primary sedimentary structures are not apparent. The unit forms alluvial fans of sediment where abandoned fluvial channels enter the east side of the Savannah River valley. Unit Qsm5 is interpreted as alluvial and fluvial sediments</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsmp4</edomv><edomvd>Sand, mud, and peat in fluvial channels (Quaternary)â€”0.3- to 3.7-m (1- to 12-ft)-thick, light-gray (N7) to medium-bluish-gray (5B 5/1) to brownish-gray (5YR 4/1) to black (N1) sand, mud, and peat in abandoned fluvial channels truncated by the westernmost terrace (Qt0) on the Savannah River flood plain. Sand grains are very fine to very coarse grained and are composed primarily of quartz. The unit is well to very well sorted. Primary sedimentary structures are not apparent. The unit is found in abandoned channels on terraces Qt1 through Qt5 shown on maps A and B. A sample of wood (WW8888; fig. 4) from this unit in gouge core C1 yielded a radiocarbon age of 41,890Â±930 14C yr BP (46,841 to 43,856 cal yr BP) (table 3). This age approaches the older limit for radiocarbon dating, and thus may be a minimum age for the sample (and a minimum age for the channel). This channel is younger than the terraces into which it has incised. Unit Qsmp4 is interpreted as fluvial and swamp deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qs2</edomv><edomvd>Sand (Quaternary)â€”0.3- to 9.1-m (1- to 30-ft)-thick, yellowish-orange (10YR 8/4) and light-gray (N7) sand. Sand grains are fine to very coarse grained and are composed of quartz (99 percent) and rock fragments (1 percent) that include mica, garnet, and epidote. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. The unit forms irregular ridges between channels. The ridges (and channels) are on (or in) terraces Qt1 through Qt5 that are bounded on the west by low-relief escarpments that trend northwest.</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm1</edomv><edomvd>Sand and mud (Holocene)â€”0.3- to 4.6-m (1- to 15-ft)-thick, white (N9) to medium-gray (N5) sand, silt, and clay. Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. The unit is found on the youngest terrace (westernmost terrace) of the Savannah River (terrace Qt0 on maps A and B) between the Savannah River and the eolian dunes (Qs1), and in most locations unit Qsm1 is associated with unit Qsm2. Unit Qsm1 is interpreted as fluvial channel point-bar deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qs1</edomv><edomvd>Sand (Quaternary)â€”0.3- to 9.1-m (1- to 30-ft)-thick, yellowish-orange (10YR 6/6) sand, overlain by a 0.1- to 0.6-m-thick veneer of brown (10YR 6/2) sand with iron-oxide coating. Sand grains are mostly fine to medium grained and are composed of quartz (99 percent) and rock fragments (1 percent) that include mica and opaque minerals; feldspar is notably absent. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. This unit forms a relatively continuous group of sand hills that are located at distances of 0 to 5 kilometers east of the modern river channel, and forms various isolated sand hills and ridges that are also located east of the modern river channel. Where discernible, the morphologies of individual hills range from parabolic shapes (with tails pointing west) to isolated circular and linear shapes. Samples from this unit have yielded 15 optically stimulated luminescence (OSL) ages (table 1). Using the preferred ages given in bold in table 1 and taking into account the reported ranges of uncertainty, 13 of these ages range from approximately 35.4 to 18.0 ka, and two of these ages range from approximately 11.0 to 9.5 ka (GAW-13 and GAW-11, table 1). The two younger ages are from relatively isolated sand hills and ridges. Unit Qs1 is interpreted as eolian dune deposits and is described in greater detail in Swezey and others (2013)</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Ngsm</edomv><edomvd>Gravel, sand, and mud (lower Pliocene?)â€”0.3-m to at least 17.4-m (1-ft to at least 57-ft)-thick, mottled light-gray (N7) and pale-reddish-brown (10R 5/4) to pale-yellowish-orange (10YR 8/6) sand and sandy mud, a few beds of gravelly sand, and a few beds of mud (silt and clay). Light-gray intervals are composed of sand (20 to 30 percent) and mud (70 to 80 percent), whereas pale-reddish-brown intervals are composed of sand (50 to 60 percent) and mud (40 to 50 percent). Most sand grains are fine to medium grained and are composed of quartz (99 percent) and rock fragments (1 percent) that include mica, garnet, and epidote. Individual beds range from poorly to moderately to well sorted. Primary sedimentary structures are not apparent at most locations, although crossbedding is visible in a few beds at one outcrop on the Savannah River. This unit, which is visible at one outcrop along the Savannah River (photographs 1 and 2), was encountered in drill core C2 and auger cores (figs. 2 and 3), and forms a high terrace that demarks the east side of the Savannah River valley. Relict meandering channels and extra-channel areas (mapped separately as Qsm3 and Qsm4) are present on the west side of this high terrace. Unit Ngsm was mapped by Doar (2008) as the Pleistocene Ladson Formation, and was mapped by Doar (2013b) as the Pleistocene Penholoway Formation. The unit is similar in both appearance and stratigraphic position to strata that are mapped collectively in Georgia as the Pliocene Cypresshead Formation (Huddlestun, 1988). Unit Ngsm is interpreted as estuarine to marginal marine sediments and beach ridges</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm4</edomv><edomvd>Sand and mud in abandoned channels (Quaternary)â€”0.3- to 10.7-m (1- to 35-ft)-thick, yellowish-orange (10YR 8/4) and light-gray (N7) sand, silt, and clay in abandoned channels on the west side of the high terrace that forms the eastern border of the Savannah River flood plain where the elevation changes abruptly from approximately 10 to &gt;15 m above sea level. This unit is mapped as deposits associated with the following two geomorphic features: (1) relict meandering channels (Qsm3), and (2) extra-channel areas that are adjacent to but outside of a channel (Qsm4). Sand grains are very fine to coarse grained and are composed of quartz (99 percent) and rock fragments (1 percent) that include mica, garnet, and epidote. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. Units Qsm3 and Qsm4 are interpreted as channel and point-bar deposits of a relict meandering fluvial system that is older than the modern Savannah River flood plain. The sizes of the relict meandering channels are similar to those of the modern Savannah River, suggesting similar flow regimes. It is presumed that the sand and mud in these relict channels are Quaternary in age</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsmp3</edomv><edomvd>Sand, mud, and peat (Quaternary)â€”0.3- to 12.2-m (1- to 40-ft)-thick, light-gray (N7) to black (N1) sand, silt, clay, and peat. Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is well to very well sorted. Primary sedimentary structures include laminations, at some locations. The unit is found in areas of low elevation and poor drainage, and rests on a series of low-relief terraces (Qt1 through Qt5). Unit Qsmp3 is interpreted as fluvial, swamp, and marsh deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm2</edomv><edomvd>Sand and mud (Holocene)â€”Two units are mapped together and are described below as unit 1 and unit 2. Both units are found on the youngest terrace (westernmost terrace) of the Savannah River (terrace Qt0 on maps A and B) Unit 1: 0.3- to 1.5-m (1- to 5-ft)-thick, white (N9) to light-yellowish- orange (10YR 8/6) sand and mud. Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. The unit forms low ridges adjacent to river channels. As described in Swezey and others (2013), this unit occurs west of and truncates the youngest eolian dunes (Qs1), which are dated at approximately 10 ka (kilo-annum, or thousand years before present). Unit 1 of Qsm2 is interpreted as levee deposits Unit 2: 0.3- to 2.1-m (1- to 7-ft)-thick, dark-yellowish-brown (10YR 4/2), brown (10Y 6/6), moderate-yellowish-orange (10YR 6/6), dark-gray (N3), and light-gray (N7) sand and mud. Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. The unit is found along the sides of small drainages that have breached levee deposits of the Savannah River. This unit occurs west of and truncates the youngest eolian dunes (Qs1), which are dated at approximately 10 ka (Swezey and others, 2013). Unit 2 of Qsm2 is interpreted as crevasse splay deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Nsm</edomv><edomvd>Sand and mud, with phosphate grains (lower Miocene)â€”At least 15.5-m (51-ft)-thick, light-olive-gray (5Y 5/2) to yellowish-gray (5Y 7/2) to grayish-olive (10Y 4/2) clay, silt, sand, and muddy sand. Sand grains are very fine to fine grained and are composed of quartz (80 to 95 percent) and phosphate (5 to 20 percent). Laminations are visible in some beds. The unit is not exposed in outcrop, but was encountered in drill core C2 and auger cores (figs. 2 and 3). The early Miocene age of this unit is constrained by biostratigraphic data from sample R6709 A in drill core C2 (table 2). Unit Nsm is interpreted as shallow marine sediments</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsmp1</edomv><edomvd>Sand, mud, and peat (Holocene)â€”0.3- to 12-meters (m) (1- to 39-feet [ft])-thick, medium-light-gray (N6) to medium-bluish-gray (5B 5/1) to moderate-brown (5YR 3/4) to black (N1) sand, silt, clay, and peat in closed depressions among the sand hills (Qs1). Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is well to very well sorted. Primary sedimentary structures include laminations, in some places. Samples from this unit in vibracore C3 (on maps A and B; fig. 4) from a closed depression yielded radiocarbon ages ranging from 8,275Â±30 14C yr BP (9,403 to 9,135 cal yr BP) to modern. Additional details about this drill core may be found in Bernhardt and others (2012). Unit Qsmp1 is interpreted as interdune swamp deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsmp2</edomv><edomvd>Sand, mud, and peat (Holocene)â€”0.3- to 1.8-m (1- to 6-ft)-thick, light-gray (N7) to black (N1) sand, silt, clay, and peat in abandoned fluvial channels on the westernmost terrace of the Savannah River (terrace Qt0 on maps A and B). Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is well to very well sorted. Primary sedimentary structures are not apparent. Unit Qsmp2 is interpreted as alluvial or swamp deposits that accumulated in abandoned fluvial channels</edomvd><edomvds>Producer defined</edomvds></edom></attrdomv></attr><attr><attrlabl>SHAPE_Area</attrlabl><attrdef>Area of feature in internal units squared.</attrdef><attrdefs>ESRI</attrdefs><attrdomv><rdom><rdommin>16.7387930713137</rdommin><rdommax>33518221.7252577</rdommax></rdom></attrdomv></attr><attr><attrlabl>SHAPE_Length</attrlabl><attrdef>Length of feature in internal units.</attrdef><attrdefs>ESRI</attrdefs><attrdomv><rdom><rdommin>15.0048870911479</rdommin><rdommax>284191.070173028</rdommax><attrunit>meter</attrunit></rdom></attrdomv></attr><attr><attrlabl>mapDesc</attrlabl><attrdef>Defines and describes geologic map units in the feature class.</attrdef><attrdefs>Producer defined</attrdefs><attrdomv><udom>Defines and describes geologic map units in the feature class. Units are defined on the basis of lithology, stratigraphic position, and interpreted depositional environment.</udom></attrdomv></attr></detailed><overview><eaover>The entity and attribute information provided here describes the tabular data associated with the data set. Please review the detailed descriptions that are provided (the individual attribute descriptions) for information on the values that appear as fields/table entries of the data set.</eaover><eadetcit>The entity and attribute information was generated by the individual and (or) agency identified as the originator of the data set. Please review the rest of the metadata record for additional details and information.</eadetcit></overview></eainfo></metadata>����&øÿÿht-gray (N7) to black (N1) sand, silt, clay, and peat in abandoned fluvial channels on the westernmost terrace of the Savannah River (terrace Qt0 on maps A and B). Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is well to very well sorted. Primary sedimentary structures are not apparent. Unit Qsmp2 is interpreted as alluvial or swamp deposits that accumulated in abandoned fluvial channels</edomvd><edomvds>Producer defined</edomvds></edom></attrdomv></attr><attr><attrlabl>SHAPE_Area</attrlabl><attrdef>Area of feature in internal units squared.</attrdef><attrdefs>ESRI</attrdefs><attrdomv><rdom><rdommin>16.7387930713137</rdommin><rdommax>33518221.7252577</rdommax></rdom></attrdomv></attr><attr><attrlabl>SHAPE_Length</attrlabl><attrdef>Length of feature in internal units.</attrdef><attrdefs>ESRI</attrdefs><attrdomv><rdom><rdommin>15.0048870911479</rdommin><rdommax>284191.070173028</rdommax><attrunit>meter</attrunit></rdom></attrdomv></attr><attr><attrlabl>mapDesc</attrlabl><attrdef>Defines and describes geologic map units in the feature class.</attrdef><attrdefs>Producer defined</attrdefs><attrdomv><udom>Defines and describes geologic map units in the feature class. Units are defined on the basis of lithology, stratigraphic position, and interpreted depositional environment.</udom></attrdomv></attr></detailed><overview><eaover>The entity and attribute information provided here describes the tabular data associated with the data set. Please review the detailed descriptions that are provided (the individual attribute descriptions) for information on the values that appear as fields/table entries of the data set.</eaover><eadetcit>The entity and attribute information was generated by the individual and (or) agency identified as the originator of the data set. Please review the rest of the metadata record for additional details and information.</eadetcit></overview></eainfo></metadata>����-����£‰/œ–­:’Í	a§��Ï’^œ¬Útÿ�¬Ê�“–�3⁄4�¿�îÊ�Ó‘�ü�‹ðÿÿtions, in some places. Samples from this unit in vibracore C3 (on maps A and B; fig. 4) from a closed depression yielded radiocarbon ages ranging from 8,275Â±30 14C yr BP (9,403 to 9,135 cal yr BP) to modern. Additional details about this drill core may be found in Bernhardt and others (2012). Unit Qsmp1 is interpreted as interdune swamp deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsmp2</edomv><edomvd>Sand, mud, and peat (Holocene)â€”0.3- to 1.8-m (1- to 6-ft)-thick, light-gray (N7) to black (N1) sand, silt, clay, and peat in abandoned fluvial channels on the westernmost terrace of the Savannah River (terrace Qt0 on maps A and B). Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is well to very well sorted. Primary sedimentary structures are not apparent. Unit Qsmp2 is interpreted as alluvial or swamp deposits that accumulated in abandoned fluvial channels</edomvd><edomvds>Producer defined</edomvds></edom></attrdomv><attalias Sync="TRUE">MapUnit</attalias><attrtype Sync="TRUE">String</attrtype><attwidth Sync="TRUE">10</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr><attr><attrlabl>SHAPE_Area</attrlabl><attrdef>Area of feature in internal units squared.</attrdef><attrdefs>ESRI</attrdefs><attrdomv><rdom><rdommin>16.7387930713137</rdommin><rdommax>33518221.7252577</rdommax></rdom><udom Sync="TRUE">Positive real numbers that are automatically generated.</udom></attrdomv><attalias Sync="TRUE">SHAPE_Area</attalias><attrtype Sync="TRUE">Double</attrtype><attwidth Sync="TRUE">8</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr><attr><attrlabl>SHAPE_Length</attrlabl><attrdef>Length of feature in internal units.</attrdef><attrdefs>ESRI</attrdefs><attrdomv><rdom><rdommin>15.0048870911479</rdommin><rdommax>284191.070173028</rdommax><attrunit>meter</attrunit></rdom><udom Sync="TRUE">Positive real numbers that are automatically generated.</udom></attrdomv><attalias Sync="TRUE">SHAPE_Length</attalias><attrtype Sync="TRUE">Double</attrtype><attwidth Sync="TRUE">8</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr><attr><attrlabl>mapDesc</attrlabl><attrdef>Defines and describes geologic map units in the feature class.</attrdef><attrdefs>Producer defined</attrdefs><attrdomv><udom>Defines and describes geologic map units in the feature class. Units are defined on the basis of lithology, stratigraphic position, and interpreted depositional environment.</udom></attrdomv><attalias Sync="TRUE">mapDesc</attalias><attrtype Sync="TRUE">String</attrtype><attwidth Sync="TRUE">250</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr></detailed><overview><eaover>The entity and attribute information provided here describes the tabular data associated with the data set. Please review the detailed descriptions that are provided (the individual attribute descriptions) for information on the values that appear as fields/table entries of the data set.</eaover><eadetcit>The entity and attribute information was generated by the individual and/or agency identified as the originator of the data set. 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value="eng"/><countryCode value="USA" Sync="TRUE"></countryCode></mdLang><mdChar><CharSetCd value="004"/></mdChar><mdHrLv><ScopeCd value="005"/></mdHrLv><mdContact><rpIndName>Christopher P Garrity</rpIndName><rpOrgName>U.S. Geological Survey, Midwest Region</rpOrgName><rpPosName>Cartographer</rpPosName><rpCntInfo><cntPhone><voiceNum>703-648-6426</voiceNum><faxNum>703-648-6419</faxNum></cntPhone><cntAddress addressType="postal"><delPoint>Mail Stop 956, 12201 Sunrise Valley Dr</delPoint><city>Reston</city><adminArea>VA</adminArea><postCode>20192</postCode><country>US</country><eMailAdd>cgarrity@usgs.gov</eMailAdd></cntAddress></rpCntInfo><role><RoleCd value="007"/></role></mdContact><mdDateSt>20190207</mdDateSt><mdStanName>ArcGIS Metadata</mdStanName><mdStanVer>1.0</mdStanVer><distInfo><distributor><distorCont><rpIndName>Christopher Swezey</rpIndName><rpOrgName>U.S. Geological Survey, Northeast Region</rpOrgName><rpPosName>Research Geologist</rpPosName><rpCntInfo><cntPhone><voiceNum>703-648-6444</voiceNum><faxNum>703-648-6953</faxNum></cntPhone><cntAddress addressType="postal"><delPoint>Mail Stop 926A, 12201 Sunrise Valley Dr</delPoint><city>Reston</city><adminArea>VA</adminArea><postCode>20192</postCode><country>US</country><eMailAdd>cswezey@usgs.gov</eMailAdd></cntAddress></rpCntInfo><role><RoleCd value="005"/></role></distorCont><distorOrdPrc><resFees>None. No fees are applicable for obtaining the data set.</resFees></distorOrdPrc><distorFormat><formatName>Digital Data</formatName></distorFormat><distorTran><onLineSrc><linkage>https://doi.org/10.3133/sim3424</linkage></onLineSrc></distorTran></distributor><distTranOps><onLineSrc><linkage>https://pubs.er.usgs.gov/sim3424</linkage></onLineSrc><onLineSrc><linkage>https://doi.org/10.3133/sim3424</linkage></onLineSrc></distTranOps><distFormat><formatName Sync="TRUE">File Geodatabase Feature Dataset</formatName></distFormat></distInfo><dataIdInfo><idCitation><resTitle>Geology of the Hardeeville NW Quadrangle and Parts of the Brighton and Pineland Quadrangles, Jasper County, South Carolina</resTitle><date><pubDate>2019-02-11</pubDate></date><citRespParty><rpOrgName>Lucy E. Edwards</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>John P. McGeehin</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>William R. Doar III</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>U.S. Geological Survey</rpOrgName><rpCntInfo><cntAddress><delPoint>Reston, Virginia</delPoint></cntAddress></rpCntInfo><role><RoleCd value="010"/></role></citRespParty><citRespParty><rpOrgName>Christopher P. Garrity</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Arthur P. Schultz</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher E. Bernhardt</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher S. Swezey</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>E. Allen Crider</rpOrgName><role><RoleCd value="006"/></role></citRespParty><presForm><fgdcGeoform>Vector Digital Data Set (Polygon)</fgdcGeoform><PresFormCd value="005" Sync="TRUE"></PresFormCd></presForm><datasetSeries><seriesName>U.S. Geological Survey Scientific Investigations Map</seriesName><issId>3424</issId></datasetSeries></idCitation><idAbs>This publication portrays the geology of the Hardeeville NW quadrangle and parts of the Brighton and Pineland quadrangles that are within Jasper County, South Carolina. This study area is located in the Atlantic Coastal Plain province, approximately 50 to 70 kilometers (km) inland from the coast. The data are compiled from geological field mapping, light detection and ranging (lidar) elevation data, cores, optically stimulated luminescence (OSL) ages, radiocarbon ages, and biostratigraphic interpretations. Most of the study area is occupied by the valley of the Savannah River, and exposures of geologic units are very limited. Traditional geologic mapping in this area is difficult because of limited access, subdued topography, extensive swamps, and abundant vegetation.</idAbs><idPurp>The purpose of this information is to provide primary data for basic and applied earth-science investigations by producing geologic maps that contribute to a comprehensive nation-wide program of geologic mapping of bedrock and surface deposits.</idPurp><idCredit>Please acknowledge U.S. Geological Survey as the source of the data.</idCredit><idStatus><ProgCd value="001"/></idStatus><idPoC><rpIndName>Christopher Swezey</rpIndName><rpOrgName>U.S. Geological Survey, Northeast Region</rpOrgName><rpPosName>Research Geologist</rpPosName><rpCntInfo><cntPhone><voiceNum>703-648-6444</voiceNum><faxNum>703-648-6953</faxNum></cntPhone><cntAddress addressType="postal"><delPoint>Mail Stop 926A, 12201 Sunrise Valley Dr</delPoint><city>Reston</city><adminArea>VA</adminArea><postCode>20192</postCode><country>US</country><eMailAdd>cswezey@usgs.gov</eMailAdd></cntAddress></rpCntInfo><role><RoleCd value="007"/></role></idPoC><resMaint><maintFreq><MaintFreqCd value="011"/></maintFreq></resMaint><placeKeys><keyword>Pineville</keyword><keyword>Brighton</keyword><keyword>Jasper</keyword><keyword>United States</keyword><keyword>Hardeeville NW</keyword><keyword>South Carolina</keyword><thesaName><resTitle>Common geographic areas</resTitle></thesaName></placeKeys><themeKeys><keyword>geoscientificInformation</keyword><thesaName><resTitle>ISO 19115 Topic Category</resTitle></thesaName></themeKeys><themeKeys><keyword>Clay or mud</keyword><keyword>Sand</keyword><keyword>Gravel</keyword><keyword>Eolian material</keyword><keyword>Peat</keyword><keyword>Terrace</keyword><thesaName><resTitle>Lithologic classification of geologic map units</resTitle></thesaName></themeKeys><themeKeys><keyword>surficial geologic units</keyword><keyword>Quaternary</keyword><keyword>geologic time periods</keyword><keyword>Pliocene</keyword><keyword>Holocene</keyword><keyword>geologic maps</keyword><keyword>Miocene</keyword><keyword>geologic contacts</keyword><thesaName><resTitle>USGS Thesaurus</resTitle></thesaName></themeKeys><searchKeys><keyword>surficial geologic units</keyword><keyword>Quaternary</keyword><keyword>geologic time periods</keyword><keyword>Clay or mud</keyword><keyword>Sand</keyword><keyword>Pliocene</keyword><keyword>Gravel</keyword><keyword>Pineville</keyword><keyword>Brighton</keyword><keyword>Holocene</keyword><keyword>Eolian material</keyword><keyword>geologic maps</keyword><keyword>geoscientificInformation</keyword><keyword>Jasper</keyword><keyword>United States</keyword><keyword>Hardeeville NW</keyword><keyword>Peat</keyword><keyword>Miocene</keyword><keyword>Terrace</keyword><keyword>geologic contacts</keyword><keyword>South Carolina</keyword></searchKeys><resConst><LegConsts><useLimit>Although all data and software released have been used by the USGS, no warranty, expressed or implied, is made by the USGS as to the accuracy of the data and related materials and (or) the functioning of the software.</useLimit><othConsts>None. Please see 'Distribution Info' for details.</othConsts></LegConsts></resConst><resConst><Consts><useLimit>Unless otherwise stated, all data, metadata and related materials are considered to satisfy the quality standards relative to the purpose for which the data were collected. Although these data and associated metadata have been reviewed for accuracy and completeness and approved for release by the U.S. Geological Survey (USGS), no warranty expressed or implied is made regarding the display or utility of the data on any other system or for general or scientific purposes, nor shall the act of distribution constitute any such warranty. Users of this geospatial data and geologic information derived there from should acknowledge the U.S. Geological Survey as the source of the data. Although software enables a user to display images at various scales, map data in this report should not be used at scales greater than 1:24,000.</useLimit></Consts></resConst><spatRpType><SpatRepTypCd value="001"/></spatRpType><dataLang><languageCode value="eng"/><countryCode value="USA" Sync="TRUE"></countryCode></dataLang><tpCat><TopicCatCd value="008"/></tpCat><envirDesc>Environment as of Metadata Creation: Microsoft Windows 7 Version 6.1 (Build 7601) Service Pack 1; Esri ArcGIS 10.6 (Build 8321) Service Pack N/A (Build N/A)</envirDesc><dataExt><exDesc>publication date</exDesc><tempEle><TempExtent><exTemp><TM_Period><tmBegin>2009-12-01</tmBegin><tmEnd>2019-02-11</tmEnd></TM_Period></exTemp></TempExtent></tempEle><geoEle/></dataExt><dataExt><geoEle><GeoBndBox><westBL>-81.2819</westBL><eastBL>-81.1246</eastBL><southBL>32.3749</southBL><northBL>32.5602</northBL></GeoBndBox></geoEle></dataExt><suppInfo>This feature class contains geologic unit boundaries for the Hardeeville NW quadrangle and parts of the Brighton and Pineland quadrangles, Jasper County, South Carolina. Digital data were compiled from source data at a scale of 1:24,000 and are not intended to be used at a larger (greater detail) scale. The release of these data will allow the general public, academia, and earth science professional to view and evaluate geologic data at the 1:24,000 scale. It is hoped that the use of these data, either by themselves or in relation to other data, may lead to new interpretations of the geology of the mapped area.</suppInfo><dataExt><geoEle><GeoBndBox esriExtentType="search"><exTypeCode Sync="TRUE">1</exTypeCode><westBL Sync="TRUE">-81.281904</westBL><eastBL Sync="TRUE">-81.124574</eastBL><northBL Sync="TRUE">32.560198</northBL><southBL Sync="TRUE">32.374940</southBL></GeoBndBox></geoEle></dataExt></dataIdInfo><dqInfo><dqScope><scpLvl><ScopeCd value="005"/></scpLvl></dqScope><report type="DQTopConsis"><evalMethDesc>Topological accuracy was tested using topology validation tools. Specific errors that were checked included: Polygon overlaps and gaps, coincident contact lines and geologic unit borders, self overlapping lines and superfluous pseudo nodes. No duplicate features exist nor duplicate points in a data string. Intersecting lines are separated into individual line segments at the point of intersection. Feature classes in the geodatabase are topologically clean.</evalMethDesc></report><report type="DQConcConsis"><measDesc>Topological accuracy was tested using topology validation tools. Specific errors that were checked included: Polygon overlaps and gaps, coincident contact lines and geologic unit borders, self overlapping lines and superfluous pseudo nodes. No duplicate features exist nor duplicate points in a data string. Intersecting lines are separated into individual line segments at the point of intersection. Feature classes in the geodatabase are topologically clean.</measDesc></report><report type="DQCompOm"><measDesc>Data set complete. No data was intentionally omitted from the source map.</measDesc></report><report type="DQQuanAttAcc"><measDesc>Attribute accuracy was tested by manual comparison of the source with hard copy printouts and/or symbolized display of the digital geologic data on an interactive computer graphic system. In addition, attributes were compared to a master set of valid geologic unit attributes.</measDesc></report><report type="DQAbsExtPosAcc" dimension="horizontal"><measDesc>A formal accuracy assessment of the horizontal positional information in the data set has not been conducted.</measDesc></report><report type="DQAbsExtPosAcc" dimension="vertical"><measDesc>A formal accuracy assessment of the vertical positional information in the data set has either not been conducted, or is not applicable.</measDesc></report><dataLineage><prcStep><stepDesc>Swezey and Schultz dug pits into these features and noted sediment composition, noted changes in vegetation assemblages associated with some of the features, and collected sediment samples for OSL dating. Swezey and Schultz also compared the sediments found in their pits with USDA soil maps of Jasper County (Stuck, 1980). Swezey and Schultz also drilled cores in the field area in order to verify vertical stratigraphic contacts.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Crider took linework, smoothed it, and made sure that the linework was topologically clean and located properly. Swezey reviewed the resulting product, and made some modifications after checking against the field data obtained by Swezey and Schultz.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>LiDAR imagery of the field area was processed by Garrity, and field data were collected by Swezey and Schultz. Schultz placed mylar on top of the LiDAR plot, consulted with field data obtained by Swezey and Schultz, and traced over features of the hillshade.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Swezey and Schultz obtained LiDAR imagery of the Hardeeville NW quadrangle and the southern half of the Brighton and Pineland quadrangles.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Christopher Swezey and Arthur Schultz obtained previously published topographic maps and previously published geologic maps of the area (Doar, 2008, 2013a, 2013b).</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Swezey and Schultz field-checked the various geomorphological features that were visible in the LiDAR imagery, paying particular attention to boundaries of the geomorphologic features.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>The LiDAR was processed by Christopher Garrity. The LiDAR imagery revealed low-relief geomorphological features that were not apparent in the previously published maps.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Crider registered and rectified the mylar over the LiDAR hillshade in ArcGIS. Schultz directly digitized the linework onscreen, using a hillshade and slope DEM from the LiDAR DEM and the registered mylar.</stepDesc><stepDateTm date="unknown"/></prcStep><dataSource><srcDesc>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, contacts and faults, or the additional supporting structural and cartographic information.</srcDesc><srcMedName><MedNameCd value="018"/></srcMedName><srcCitatn><resTitle>A revision of the lithostratigraphic units of the Coastal Plain of Georgia</resTitle><resAltTitle>Huddlestun, 1988</resAltTitle><date><pubDate>1988-01-01</pubDate></date><citRespParty><rpOrgName>Paul F. Huddlestun</rpOrgName><role><RoleCd value="006"/></role></citRespParty><presForm><fgdcGeoform>publication</fgdcGeoform></presForm><datasetSeries><seriesName>Georgia Geologic Bulletin</seriesName><issId>no. 104</issId></datasetSeries><otherCitDet>Huddlestun, P.F., 1988, A revision of the lithostratigraphic units of the Coastal Plain of Georgiaâ€”The Miocene through Holocene: Georgia Geologic Survey Bulletin 104, 162 p. [Also available at https://epd.georgia.gov/sites/epd.georgia.gov/files/related_files/site_page/B-104.pdf.]</otherCitDet><citOnlineRes><linkage>https://epd.georgia.gov/sites/epd.georgia.gov/files/related_files/site_page/B-104.pdf</linkage></citOnlineRes></srcCitatn><srcExt><exDesc>publication date</exDesc><tempEle><TempExtent><exTemp><TM_Instant><tmPosition>1988-01-01</tmPosition></TM_Instant></exTemp></TempExtent></tempEle></srcExt></dataSource><dataSource><srcDesc>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, contacts and faults, or the additional supporting structural and cartographic information.</srcDesc><srcMedName><MedNameCd value="018"/></srcMedName><srcScale><rfDenom>0</rfDenom></srcScale><srcCitatn><resTitle>Palynological studies reveal Holocene climate changes in a forested flood plain wetland, Savannah River valley, South Carolina (USA)</resTitle><resAltTitle>Bernhardt and others, 2012</resAltTitle><date><pubDate>2012-01-01</pubDate></date><citRespParty><rpOrgName>Arthur P. Schultz</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher Bernhardt</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher S. Swezey</rpOrgName><role><RoleCd value="006"/></role></citRespParty><presForm><fgdcGeoform>publication</fgdcGeoform></presForm><datasetSeries><seriesName>Geological Society of America Abstracts with Programs</seriesName><issId>v. 44, no. 7</issId></datasetSeries><otherCitDet>Bernhardt, C., Swezey, C.S., and Schultz, A.P., 2012, Palynological studies reveal Holocene climate changes in a forested flood plain wetland, Savannah River valley, South Carolina (USA) [abs.]: Geological Society of America Abstracts with Programs, v. 44, no. 7, p. 423. [Also available at https://gsa.confex.com/gsa/2012AM/webprogram/Paper211715.html.]</otherCitDet><citOnlineRes><linkage>https://gsa.confex.com/gsa/2012AM/webprogram/Paper211715.html</linkage></citOnlineRes></srcCitatn><srcExt><exDesc>publication date</exDesc><tempEle><TempExtent><exTemp><TM_Instant><tmPosition>2012-01-01</tmPosition></TM_Instant></exTemp></TempExtent></tempEle></srcExt></dataSource><dataSource><srcDesc>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, contacts and faults, or the additional supporting structural and cartographic information.</srcDesc><srcMedName><MedNameCd value="018"/></srcMedName><srcCitatn><resTitle>Quaternary eolian dunes in the Savannah River Valley, Jasper County, South Carolina, USA</resTitle><resAltTitle>Swezey and others, 2013</resAltTitle><date><pubDate>2017-01-20</pubDate></date><citRespParty><rpOrgName>Cambridge University Press (CUP)</rpOrgName><rpCntInfo><cntAddress><delPoint>n/a</delPoint></cntAddress></rpCntInfo><role><RoleCd value="010"/></role></citRespParty><citRespParty><rpOrgName>Arthur P. Schultz</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>John P. McGeehin</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher P. Garrity</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Wilma AlemÃ¡n GonzÃ¡lez</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher S. Swezey</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher E. Bernhardt</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Shannon A. Mahan</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>William R. Doar</rpOrgName><role><RoleCd value="006"/></role></citRespParty><presForm><fgdcGeoform>publication</fgdcGeoform></presForm><datasetSeries><seriesName>Quaternary Research</seriesName><issId>v. 80, no. 02</issId></datasetSeries><otherCitDet>Swezey, C.S., Schultz, A.P., AlemÃ¡n GonzÃ¡lez, W.B., Bernhardt, C.E., Doar, W.R., III, Garrity, C.P., Mahan, S.A., and McGeehin, J.P., 2013, Quaternary eolian dunes in the Savannah River Valley, Jasper County, South Carolina, USA: Quaternary Research, v. 80, no. 2, p. 250â€“264. [Also available at http://www.sciencedirect.com/science/article/pii/S0033589413000719.]</otherCitDet><citOnlineRes><linkage>http://dx.doi.org/10.1016/j.yqres.2013.06.007</linkage></citOnlineRes></srcCitatn><srcExt><exDesc>publication date</exDesc><tempEle><TempExtent><exTemp><TM_Instant><tmPosition>2017-01-01</tmPosition></TM_Instant></exTemp></TempExtent></tempEle></srcExt></dataSource></dataLineage></dqInfo><spatRepInfo><VectSpatRep><geometObjs Name="SurficialContacts"><geoObjTyp><GeoObjTypCd value="002" Sync="TRUE"></GeoObjTypCd></geoObjTyp><geoObjCnt Sync="TRUE">717</geoObjCnt></geometObjs><topLvl><TopoLevCd value="001" Sync="TRUE"></TopoLevCd></topLvl><geometObjs Name="SurficialPolygons"><geoObjTyp><GeoObjTypCd value="002" Sync="TRUE"></GeoObjTypCd></geoObjTyp><geoObjCnt Sync="TRUE">695</geoObjCnt></geometObjs></VectSpatRep></spatRepInfo><mdHrLvName Sync="TRUE">dataset</mdHrLvName><refSysInfo><RefSystem><refSysID><identCode code="26917" Sync="TRUE"></identCode><idCodeSpace Sync="TRUE">EPSG</idCodeSpace><idVersion Sync="TRUE">6.13(3.0.1)</idVersion></refSysID></RefSystem></refSysInfo><spdoinfo><ptvctinf><esriterm Name="SurficialContacts"><efeatyp Sync="TRUE">Simple</efeatyp><efeageom code="3" Sync="TRUE"></efeageom><esritopo Sync="TRUE">FALSE</esritopo><efeacnt Sync="TRUE">717</efeacnt><spindex Sync="TRUE">TRUE</spindex><linrefer Sync="TRUE">FALSE</linrefer></esriterm><esriterm Name="SurficialPolygons"><efeatyp Sync="TRUE">Simple</efeatyp><efeageom code="4" Sync="TRUE"></efeageom><esritopo Sync="TRUE">FALSE</esritopo><efeacnt Sync="TRUE">695</efeacnt><spindex Sync="TRUE">TRUE</spindex><linrefer Sync="TRUE">FALSE</linrefer></esriterm></ptvctinf></spdoinfo></metadata>�����Àÿÿ, (2) a sample of sand (GAW-14; table 1) collected from a depth of 70 cm below the surface of terrace Qt4 yielded a preferred OSL age of 24.2Â±1.2 ka, and (3) a sample of sandy mud (GAW-28; table 1) collected from a depth of 84 cm below the surface of terrace Qt4 yielded a preferred OSL age 23.6Â±2.1 ka. Unit Qs3 is interpreted as fluvial terrace deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm3</edomv><edomvd>Sand and mud in abandoned channels (Quaternary)â€”0.3- to 10.7-m (1- to 35-ft)-thick, yellowish-orange (10YR 8/4) and light-gray (N7) sand, silt, and clay in abandoned channels on the west side of the high terrace that forms the eastern border of the Savannah River flood plain where the elevation changes abruptly from approximately 10 to &gt;15 m above sea level. This unit is mapped as deposits associated with the following two geomorphic features: (1) relict meandering channels (Qsm3), and (2) extra-channel areas that are adjacent to but outside of a channel (Qsm4). Sand grains are very fine to coarse grained and are composed of quartz (99 percent) and rock fragments (1 percent) that include mica, garnet, and epidote. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. Units Qsm3 and Qsm4 are interpreted as channel and point-bar deposits of a relict meandering fluvial system that is older than the modern Savannah River flood plain. The sizes of the relict meandering channels are similar to those of the modern Savannah River, suggesting similar flow regimes. It is presumed that the sand and mud in these relict channels are Quaternary in age</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qgsm</edomv><edomvd>Gravel, sand, and mud (Pleistocene)â€”3.0- to 9.1-m (10- to 30-ft)-thick, sand and gravelly sand that fines upward to sand and then muddy sand. The lower part (sand and gravelly sand) is very light gray (N8) to medium gray (N5), whereas the upper part is mottled light-brown (5YR 5/6), pale-brown (5YR 5/2), yellowish-orange (10YR 4/6), yellowish-gray (5YR 7/2), and moderate-greenish-yellow (10Y 7/4) muddy sand. Gravel in the lower part is granules and pebbles of quartz and feldspar. Sand grains in the lower part are fine to very coarse grained and are composed of quartz (98 percent) and rock fragments (2 percent) that include mica, garnet, epidote, and amphibole. Sand grains in the upper part are very fine to fine grained and are composed of quartz (98 percent) and rock fragments (2 percent) that include mica and opaque minerals. The lower part of the unit is poorly to moderately sorted, whereas the upper part of the unit is moderately sorted to well sorted. Primary sedimentary structures are not apparent. Unit Qgsm forms an overall fining-upward sequence and is interpreted as a fluvial deposit. A terrace is formed on this unit in the southeasternmost part of the study area and appears to be greatly weathered. On the basis of elevation and geomorphological expression in the light detection and ranging (lidar) image (map B), the unit is thought to be older than terraces Qt1 through Qt5</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm5</edomv><edomvd>Sand and mud (Pleistocene)â€”0.3- to 9.1-m (1- to 30-ft)-thick, medium-light-gray (N6) to light-gray (N7) sand and muddy sand. Sand grains are fine to coarse grained and are composed predominantly of quartz. The unit is poorly to well sorted. Primary sedimentary structures are not apparent. The unit forms alluvial fans of sediment where abandoned fluvial channels enter the east side of the Savannah River valley. Unit Qsm5 is interpreted as alluvial and fluvial sediments</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsmp4</edomv><edomvd>Sand, mud, and peat in fluvial channels (Quaternary)â€”0.3- to 3.7-m (1- to 12-ft)-thick, light-gray (N7) to medium-bluish-gray (5B 5/1) to brownish-gray (5YR 4/1) to black (N1) sand, mud, and peat in abandoned fluvial channels truncated by the westernmost terrace (Qt0) on the Savannah River flood plain. Sand grains are very fine to very coarse grained and are composed primarily of quartz. The unit is well to very well sorted. Primary sedimentary structures are not apparent. The unit is found in abandoned channels on terraces Qt1 through Qt5 shown on maps A and B. A sample of wood (WW8888; fig. 4) from this unit in gouge core C1 yielded a radiocarbon age of 41,890Â±930 14C yr BP (46,841 to 43,856 cal yr BP) (table 3). This age approaches the older limit for radiocarbon dating, and thus may be a minimum age for the sample (and a minimum age for the channel). This channel is younger than the terraces into which it has incised. Unit Qsmp4 is interpreted as fluvial and swamp deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qs2</edomv><edomvd>Sand (Quaternary)â€”0.3- to 9.1-m (1- to 30-ft)-thick, yellowish-orange (10YR 8/4) and light-gray (N7) sand. Sand grains are fine to very coarse grained and are composed of quartz (99 percent) and rock fragments (1 percent) that include mica, garnet, and epidote. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. The unit forms irregular ridges between channels. The ridges (and channels) are on (or in) terraces Qt1 through Qt5 that are bounded on the west by low-relief escarpments that trend northwest.</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm1</edomv><edomvd>Sand and mud (Holocene)â€”0.3- to 4.6-m (1- to 15-ft)-thick, white (N9) to medium-gray (N5) sand, silt, and clay. Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. The unit is found on the youngest terrace (westernmost terrace) of the Savannah River (terrace Qt0 on maps A and B) between the Savannah River and the eolian dunes (Qs1), and in most locations unit Qsm1 is associated with unit Qsm2. Unit Qsm1 is interpreted as fluvial channel point-bar deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qs1</edomv><edomvd>Sand (Quaternary)â€”0.3- to 9.1-m (1- to 30-ft)-thick, yellowish-orange (10YR 6/6) sand, overlain by a 0.1- to 0.6-m-thick veneer of brown (10YR 6/2) sand with iron-oxide coating. Sand grains are mostly fine to medium grained and are composed of quartz (99 percent) and rock fragments (1 percent) that include mica and opaque minerals; feldspar is notably absent. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. This unit forms a relatively continuous group of sand hills that are located at distances of 0 to 5 kilometers east of the modern river channel, and forms various isolated sand hills and ridges that are also located east of the modern river channel. Where discernible, the morphologies of individual hills range from parabolic shapes (with tails pointing west) to isolated circular and linear shapes. Samples from this unit have yielded 15 optically stimulated luminescence (OSL) ages (table 1). Using the preferred ages given in bold in table 1 and taking into account the reported ranges of uncertainty, 13 of these ages range from approximately 35.4 to 18.0 ka, and two of these ages range from approximately 11.0 to 9.5 ka (GAW-13 and GAW-11, table 1). The two younger ages are from relatively isolated sand hills and ridges. Unit Qs1 is interpreted as eolian dune deposits and is described in greater detail in Swezey and others (2013)</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Ngsm</edomv><edomvd>Gravel, sand, and mud (lower Pliocene?)â€”0.3-m to at least 17.4-m (1-ft to at least 57-ft)-thick, mottled light-gray (N7) and pale-reddish-brown (10R 5/4) to pale-yellowish-orange (10YR 8/6) sand and sandy mud, a few beds of gravelly sand, and a few beds of mud (silt and clay). Light-gray intervals are composed of sand (20 to 30 percent) and mud (70 to 80 percent), whereas pale-reddish-brown intervals are composed of sand (50 to 60 percent) and mud (40 to 50 percent). Most sand grains are fine to medium grained and are composed of quartz (99 percent) and rock fragments (1 percent) that include mica, garnet, and epidote. Individual beds range from poorly to moderately to well sorted. Primary sedimentary structures are not apparent at most locations, although crossbedding is visible in a few beds at one outcrop on the Savannah River. This unit, which is visible at one outcrop along the Savannah River (photographs 1 and 2), was encountered in drill core C2 and auger cores (figs. 2 and 3), and forms a high terrace that demarks the east side of the Savannah River valley. Relict meandering channels and extra-channel areas (mapped separately as Qsm3 and Qsm4) are present on the west side of this high terrace. Unit Ngsm was mapped by Doar (2008) as the Pleistocene Ladson Formation, and was mapped by Doar (2013b) as the Pleistocene Penholoway Formation. The unit is similar in both appearance and stratigraphic position to strata that are mapped collectively in Georgia as the Pliocene Cypresshead Formation (Huddlestun, 1988). Unit Ngsm is interpreted as estuarine to marginal marine sediments and beach ridges</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm4</edomv><edomvd>Sand and mud in abandoned channels (Quaternary)â€”0.3- to 10.7-m (1- to 35-ft)-thick, yellowish-orange (10YR 8/4) and light-gray (N7) sand, silt, and clay in abandoned channels on the west side of the high terrace that forms the eastern border of the Savannah River flood plain where the elevation changes abruptly from approximately 10 to &gt;15 m above sea level. This unit is mapped as deposits associated with the following two geomorphic features: (1) relict meandering channels (Qsm3), and (2) extra-channel areas that are adjacent to but outside of a channel (Qsm4). Sand grains are very fine to coarse grained and are composed of quartz (99 percent) and rock fragments (1 percent) that include mica, garnet, and epidote. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. Units Qsm3 and Qsm4 are interpreted as channel and point-bar deposits of a relict meandering fluvial system that is older than the modern Savannah River flood plain. The sizes of the relict meandering channels are similar to those of the modern Savannah River, suggesting similar flow regimes. It is presumed that the sand and mud in these relict channels are Quaternary in age</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsmp3</edomv><edomvd>Sand, mud, and peat (Quaternary)â€”0.3- to 12.2-m (1- to 40-ft)-thick, light-gray (N7) to black (N1) sand, silt, clay, and peat. Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is well to very well sorted. Primary sedimentary structures include laminations, at some locations. The unit is found in areas of low elevation and poor drainage, and rests on a series of low-relief terraces (Qt1 through Qt5). Unit Qsmp3 is interpreted as fluvial, swamp, and marsh deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm2</edomv><edomvd>Sand and mud (Holocene)â€”Two units are mapped together and are described below as unit 1 and unit 2. Both units are found on the youngest terrace (westernmost terrace) of the Savannah River (terrace Qt0 on maps A and B) Unit 1: 0.3- to 1.5-m (1- to 5-ft)-thick, white (N9) to light-yellowish- orange (10YR 8/6) sand and mud. Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. The unit forms low ridges adjacent to river channels. As described in Swezey and others (2013), this unit occurs west of and truncates the youngest eolian dunes (Qs1), which are dated at approximately 10 ka (kilo-annum, or thousand years before present). Unit 1 of Qsm2 is interpreted as levee deposits Unit 2: 0.3- to 2.1-m (1- to 7-ft)-thick, dark-yellowish-brown (10YR 4/2), brown (10Y 6/6), moderate-yellowish-orange (10YR 6/6), dark-gray (N3), and light-gray (N7) sand and mud. Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. The unit is found along the sides of small drainages that have breached levee deposits of the Savannah River. This unit occurs west of and truncates the youngest eolian dunes (Qs1), which are dated at approximately 10 ka (Swezey and others, 2013). Unit 2 of Qsm2 is interpreted as crevasse splay deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Nsm</edomv><edomvd>Sand and mud, with phosphate grains (lower Miocene)â€”At least 15.5-m (51-ft)-thick, light-olive-gray (5Y 5/2) to yellowish-gray (5Y 7/2) to grayish-olive (10Y 4/2) clay, silt, sand, and muddy sand. Sand grains are very fine to fine grained and are composed of quartz (80 to 95 percent) and phosphate (5 to 20 percent). Laminations are visible in some beds. The unit is not exposed in outcrop, but was encountered in drill core C2 and auger cores (figs. 2 and 3). The early Miocene age of this unit is constrained by biostratigraphic data from sample R6709 A in drill core C2 (table 2). Unit Nsm is interpreted as shallow marine sediments</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsmp1</edomv><edomvd>Sand, mud, and peat (Holocene)â€”0.3- to 12-meters (m) (1- to 39-feet [ft])-thick, medium-light-gray (N6) to medium-bluish-gray (5B 5/1) to moderate-brown (5YR 3/4) to black (N1) sand, silt, clay, and peat in closed depressions among the sand hills (Qs1). Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is well to very well sorted. Primary sedimentary structures include laminations, in some places. Samples from this unit in vibracore C3 (on maps A and B; fig. 4) from a closed depression yielded radiocarbon ages ranging from 8,275Â±30 14C yr BP (9,403 to 9,135 cal yr BP) to modern. Additional details about this drill core may be found in Bernhardt and others (2012). Unit Qsmp1 is interpreted as interdune swamp deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsmp2</edomv><edomvd>Sand, mud, and peat (Holocene)â€”0.3- to 1.8-m (1- to 6-ft)-thick, light-gray (N7) to black (N1) sand, silt, clay, and peat in abandoned fluvial channels on the westernmost terrace of the Savannah River (terrace Qt0 on maps A and B). Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is well to very well sorted. Primary sedimentary structures are not apparent. 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value="eng"/><countryCode value="USA" Sync="TRUE"></countryCode></mdLang><mdChar><CharSetCd value="004"/></mdChar><mdHrLv><ScopeCd value="005"/></mdHrLv><mdContact><rpIndName>Christopher P Garrity</rpIndName><rpOrgName>U.S. Geological Survey, Midwest Region</rpOrgName><rpPosName>Cartographer</rpPosName><rpCntInfo><cntPhone><voiceNum>703-648-6426</voiceNum><faxNum>703-648-6419</faxNum></cntPhone><cntAddress addressType="postal"><delPoint>Mail Stop 956, 12201 Sunrise Valley Dr</delPoint><city>Reston</city><adminArea>VA</adminArea><postCode>20192</postCode><country>US</country><eMailAdd>cgarrity@usgs.gov</eMailAdd></cntAddress></rpCntInfo><role><RoleCd value="007"/></role></mdContact><mdDateSt>20190207</mdDateSt><mdStanName>ArcGIS Metadata</mdStanName><mdStanVer>1.0</mdStanVer><distInfo><distributor><distorCont><rpIndName>Christopher Swezey</rpIndName><rpOrgName>U.S. Geological Survey, Northeast Region</rpOrgName><rpPosName>Research Geologist</rpPosName><rpCntInfo><cntPhone><voiceNum>703-648-6444</voiceNum><faxNum>703-648-6953</faxNum></cntPhone><cntAddress addressType="postal"><delPoint>Mail Stop 926A, 12201 Sunrise Valley Dr</delPoint><city>Reston</city><adminArea>VA</adminArea><postCode>20192</postCode><country>US</country><eMailAdd>cswezey@usgs.gov</eMailAdd></cntAddress></rpCntInfo><role><RoleCd value="005"/></role></distorCont><distorOrdPrc><resFees>None. No fees are applicable for obtaining the data set.</resFees></distorOrdPrc><distorFormat><formatName>Digital Data</formatName></distorFormat><distorTran><onLineSrc><linkage>https://doi.org/10.3133/sim3424</linkage></onLineSrc></distorTran></distributor><distTranOps><onLineSrc><linkage>https://pubs.er.usgs.gov/sim3424</linkage></onLineSrc><onLineSrc><linkage>https://doi.org/10.3133/sim3424</linkage></onLineSrc></distTranOps><distFormat><formatName Sync="TRUE">File Geodatabase Feature Class</formatName></distFormat></distInfo><dataIdInfo><idCitation><resTitle>Geology of the Hardeeville NW Quadrangle and Parts of the Brighton and Pineland Quadrangles, Jasper County, South Carolina</resTitle><date><pubDate>2019-02-11</pubDate></date><citRespParty><rpOrgName>Lucy E. Edwards</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>John P. McGeehin</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>William R. Doar III</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>U.S. Geological Survey</rpOrgName><rpCntInfo><cntAddress><delPoint>Reston, Virginia</delPoint></cntAddress></rpCntInfo><role><RoleCd value="010"/></role></citRespParty><citRespParty><rpOrgName>Christopher P. Garrity</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Arthur P. Schultz</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher E. Bernhardt</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher S. Swezey</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>E. Allen Crider</rpOrgName><role><RoleCd value="006"/></role></citRespParty><presForm><fgdcGeoform>Vector Digital Data Set (Polygon)</fgdcGeoform><PresFormCd value="005" Sync="TRUE"></PresFormCd></presForm><datasetSeries><seriesName>U.S. Geological Survey Scientific Investigations Map</seriesName><issId>3424</issId></datasetSeries></idCitation><idAbs>This publication portrays the geology of the Hardeeville NW quadrangle and parts of the Brighton and Pineland quadrangles that are within Jasper County, South Carolina. This study area is located in the Atlantic Coastal Plain province, approximately 50 to 70 kilometers (km) inland from the coast. The data are compiled from geological field mapping, light detection and ranging (lidar) elevation data, cores, optically stimulated luminescence (OSL) ages, radiocarbon ages, and biostratigraphic interpretations. Most of the study area is occupied by the valley of the Savannah River, and exposures of geologic units are very limited. Traditional geologic mapping in this area is difficult because of limited access, subdued topography, extensive swamps, and abundant vegetation.</idAbs><idPurp>The purpose of this information is to provide primary data for basic and applied earth-science investigations by producing geologic maps that contribute to a comprehensive nation-wide program of geologic mapping of bedrock and surface deposits.</idPurp><idCredit>Please acknowledge U.S. Geological Survey as the source of the data.</idCredit><idStatus><ProgCd value="001"/></idStatus><idPoC><rpIndName>Christopher Swezey</rpIndName><rpOrgName>U.S. Geological Survey, Northeast Region</rpOrgName><rpPosName>Research Geologist</rpPosName><rpCntInfo><cntPhone><voiceNum>703-648-6444</voiceNum><faxNum>703-648-6953</faxNum></cntPhone><cntAddress addressType="postal"><delPoint>Mail Stop 926A, 12201 Sunrise Valley Dr</delPoint><city>Reston</city><adminArea>VA</adminArea><postCode>20192</postCode><country>US</country><eMailAdd>cswezey@usgs.gov</eMailAdd></cntAddress></rpCntInfo><role><RoleCd value="007"/></role></idPoC><resMaint><maintFreq><MaintFreqCd value="011"/></maintFreq></resMaint><placeKeys><keyword>Pineville</keyword><keyword>Brighton</keyword><keyword>Jasper</keyword><keyword>United States</keyword><keyword>Hardeeville NW</keyword><keyword>South Carolina</keyword><thesaName><resTitle>Common geographic areas</resTitle></thesaName></placeKeys><themeKeys><keyword>geoscientificInformation</keyword><thesaName><resTitle>ISO 19115 Topic Category</resTitle></thesaName></themeKeys><themeKeys><keyword>Clay or mud</keyword><keyword>Sand</keyword><keyword>Gravel</keyword><keyword>Eolian material</keyword><keyword>Peat</keyword><keyword>Terrace</keyword><thesaName><resTitle>Lithologic classification of geologic map units</resTitle></thesaName></themeKeys><themeKeys><keyword>surficial geologic units</keyword><keyword>Quaternary</keyword><keyword>geologic time periods</keyword><keyword>Pliocene</keyword><keyword>Holocene</keyword><keyword>geologic maps</keyword><keyword>Miocene</keyword><keyword>geologic contacts</keyword><thesaName><resTitle>USGS Thesaurus</resTitle></thesaName></themeKeys><searchKeys><keyword>surficial geologic units</keyword><keyword>Quaternary</keyword><keyword>geologic time periods</keyword><keyword>Clay or mud</keyword><keyword>Sand</keyword><keyword>Pliocene</keyword><keyword>Gravel</keyword><keyword>Pineville</keyword><keyword>Brighton</keyword><keyword>Holocene</keyword><keyword>Eolian material</keyword><keyword>geologic maps</keyword><keyword>geoscientificInformation</keyword><keyword>Jasper</keyword><keyword>United States</keyword><keyword>Hardeeville NW</keyword><keyword>Peat</keyword><keyword>Miocene</keyword><keyword>Terrace</keyword><keyword>geologic contacts</keyword><keyword>South Carolina</keyword></searchKeys><resConst><LegConsts><useLimit>Although all data and software released have been used by the USGS, no warranty, expressed or implied, is made by the USGS as to the accuracy of the data and related materials and (or) the functioning of the software.</useLimit><othConsts>None. Please see 'Distribution Info' for details.</othConsts></LegConsts></resConst><resConst><Consts><useLimit>Unless otherwise stated, all data, metadata and related materials are considered to satisfy the quality standards relative to the purpose for which the data were collected. Although these data and associated metadata have been reviewed for accuracy and completeness and approved for release by the U.S. Geological Survey (USGS), no warranty expressed or implied is made regarding the display or utility of the data on any other system or for general or scientific purposes, nor shall the act of distribution constitute any such warranty. Users of this geospatial data and geologic information derived there from should acknowledge the U.S. Geological Survey as the source of the data. Although software enables a user to display images at various scales, map data in this report should not be used at scales greater than 1:24,000.</useLimit></Consts></resConst><spatRpType><SpatRepTypCd value="001"/></spatRpType><dataLang><languageCode value="eng"/><countryCode value="USA" Sync="TRUE"></countryCode></dataLang><tpCat><TopicCatCd value="008"/></tpCat><envirDesc>Environment as of Metadata Creation: Microsoft Windows 7 Version 6.1 (Build 7601) Service Pack 1; Esri ArcGIS 10.6 (Build 8321) Service Pack N/A (Build N/A)</envirDesc><dataExt><exDesc>publication date</exDesc><tempEle><TempExtent><exTemp><TM_Period><tmBegin>2009-12-01</tmBegin><tmEnd>2019-02-11</tmEnd></TM_Period></exTemp></TempExtent></tempEle><geoEle/></dataExt><dataExt><geoEle><GeoBndBox><westBL>-81.2819</westBL><eastBL>-81.1246</eastBL><southBL>32.3749</southBL><northBL>32.5602</northBL></GeoBndBox></geoEle></dataExt><suppInfo>This feature class contains geologic unit boundaries for the Hardeeville NW quadrangle and parts of the Brighton and Pineland quadrangles, Jasper County, South Carolina. Digital data were compiled from source data at a scale of 1:24,000 and are not intended to be used at a larger (greater detail) scale. The release of these data will allow the general public, academia, and earth science professional to view and evaluate geologic data at the 1:24,000 scale. It is hoped that the use of these data, either by themselves or in relation to other data, may lead to new interpretations of the geology of the mapped area.</suppInfo><dataExt><geoEle><GeoBndBox esriExtentType="search"><exTypeCode Sync="TRUE">1</exTypeCode><westBL Sync="TRUE">-81.281904</westBL><eastBL Sync="TRUE">-81.124574</eastBL><northBL Sync="TRUE">32.560198</northBL><southBL Sync="TRUE">32.374940</southBL></GeoBndBox></geoEle></dataExt></dataIdInfo><dqInfo><dqScope><scpLvl><ScopeCd value="005"/></scpLvl></dqScope><report type="DQTopConsis"><evalMethDesc>Topological accuracy was tested using topology validation tools. Specific errors that were checked included: Polygon overlaps and gaps, coincident contact lines and geologic unit borders, self overlapping lines and superfluous pseudo nodes. No duplicate features exist nor duplicate points in a data string. Intersecting lines are separated into individual line segments at the point of intersection. Feature classes in the geodatabase are topologically clean.</evalMethDesc></report><report type="DQConcConsis"><measDesc>Topological accuracy was tested using topology validation tools. Specific errors that were checked included: Polygon overlaps and gaps, coincident contact lines and geologic unit borders, self overlapping lines and superfluous pseudo nodes. No duplicate features exist nor duplicate points in a data string. Intersecting lines are separated into individual line segments at the point of intersection. Feature classes in the geodatabase are topologically clean.</measDesc></report><report type="DQCompOm"><measDesc>Data set complete. No data was intentionally omitted from the source map.</measDesc></report><report type="DQQuanAttAcc"><measDesc>Attribute accuracy was tested by manual comparison of the source with hard copy printouts and/or symbolized display of the digital geologic data on an interactive computer graphic system. In addition, attributes were compared to a master set of valid geologic unit attributes.</measDesc></report><report type="DQAbsExtPosAcc" dimension="horizontal"><measDesc>A formal accuracy assessment of the horizontal positional information in the data set has not been conducted.</measDesc></report><report type="DQAbsExtPosAcc" dimension="vertical"><measDesc>A formal accuracy assessment of the vertical positional information in the data set has either not been conducted, or is not applicable.</measDesc></report><dataLineage><prcStep><stepDesc>Swezey and Schultz dug pits into these features and noted sediment composition, noted changes in vegetation assemblages associated with some of the features, and collected sediment samples for OSL dating. Swezey and Schultz also compared the sediments found in their pits with USDA soil maps of Jasper County (Stuck, 1980). Swezey and Schultz also drilled cores in the field area in order to verify vertical stratigraphic contacts.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Crider took linework, smoothed it, and made sure that the linework was topologically clean and located properly. Swezey reviewed the resulting product, and made some modifications after checking against the field data obtained by Swezey and Schultz.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>LiDAR imagery of the field area was processed by Garrity, and field data were collected by Swezey and Schultz. Schultz placed mylar on top of the LiDAR plot, consulted with field data obtained by Swezey and Schultz, and traced over features of the hillshade.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Swezey and Schultz obtained LiDAR imagery of the Hardeeville NW quadrangle and the southern half of the Brighton and Pineland quadrangles.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Christopher Swezey and Arthur Schultz obtained previously published topographic maps and previously published geologic maps of the area (Doar, 2008, 2013a, 2013b).</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Swezey and Schultz field-checked the various geomorphological features that were visible in the LiDAR imagery, paying particular attention to boundaries of the geomorphologic features.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>The LiDAR was processed by Christopher Garrity. The LiDAR imagery revealed low-relief geomorphological features that were not apparent in the previously published maps.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Crider registered and rectified the mylar over the LiDAR hillshade in ArcGIS. Schultz directly digitized the linework onscreen, using a hillshade and slope DEM from the LiDAR DEM and the registered mylar.</stepDesc><stepDateTm date="unknown"/></prcStep><dataSource><srcDesc>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, contacts and faults, or the additional supporting structural and cartographic information.</srcDesc><srcMedName><MedNameCd value="018"/></srcMedName><srcCitatn><resTitle>A revision of the lithostratigraphic units of the Coastal Plain of Georgia</resTitle><resAltTitle>Huddlestun, 1988</resAltTitle><date><pubDate>1988-01-01</pubDate></date><citRespParty><rpOrgName>Paul F. Huddlestun</rpOrgName><role><RoleCd value="006"/></role></citRespParty><presForm><fgdcGeoform>publication</fgdcGeoform></presForm><datasetSeries><seriesName>Georgia Geologic Bulletin</seriesName><issId>no. 104</issId></datasetSeries><otherCitDet>Huddlestun, P.F., 1988, A revision of the lithostratigraphic units of the Coastal Plain of Georgiaâ€”The Miocene through Holocene: Georgia Geologic Survey Bulletin 104, 162 p. [Also available at https://epd.georgia.gov/sites/epd.georgia.gov/files/related_files/site_page/B-104.pdf.]</otherCitDet><citOnlineRes><linkage>https://epd.georgia.gov/sites/epd.georgia.gov/files/related_files/site_page/B-104.pdf</linkage></citOnlineRes></srcCitatn><srcExt><exDesc>publication date</exDesc><tempEle><TempExtent><exTemp><TM_Instant><tmPosition>1988-01-01</tmPosition></TM_Instant></exTemp></TempExtent></tempEle></srcExt></dataSource><dataSource><srcDesc>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, contacts and faults, or the additional supporting structural and cartographic information.</srcDesc><srcMedName><MedNameCd value="018"/></srcMedName><srcScale><rfDenom>0</rfDenom></srcScale><srcCitatn><resTitle>Palynological studies reveal Holocene climate changes in a forested flood plain wetland, Savannah River valley, South Carolina (USA)</resTitle><resAltTitle>Bernhardt and others, 2012</resAltTitle><date><pubDate>2012-01-01</pubDate></date><citRespParty><rpOrgName>Arthur P. Schultz</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher Bernhardt</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher S. Swezey</rpOrgName><role><RoleCd value="006"/></role></citRespParty><presForm><fgdcGeoform>publication</fgdcGeoform></presForm><datasetSeries><seriesName>Geological Society of America Abstracts with Programs</seriesName><issId>v. 44, no. 7</issId></datasetSeries><otherCitDet>Bernhardt, C., Swezey, C.S., and Schultz, A.P., 2012, Palynological studies reveal Holocene climate changes in a forested flood plain wetland, Savannah River valley, South Carolina (USA) [abs.]: Geological Society of America Abstracts with Programs, v. 44, no. 7, p. 423. [Also available at https://gsa.confex.com/gsa/2012AM/webprogram/Paper211715.html.]</otherCitDet><citOnlineRes><linkage>https://gsa.confex.com/gsa/2012AM/webprogram/Paper211715.html</linkage></citOnlineRes></srcCitatn><srcExt><exDesc>publication date</exDesc><tempEle><TempExtent><exTemp><TM_Instant><tmPosition>2012-01-01</tmPosition></TM_Instant></exTemp></TempExtent></tempEle></srcExt></dataSource><dataSource><srcDesc>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, contacts and faults, or the additional supporting structural and cartographic information.</srcDesc><srcMedName><MedNameCd value="018"/></srcMedName><srcCitatn><resTitle>Quaternary eolian dunes in the Savannah River Valley, Jasper County, South Carolina, USA</resTitle><resAltTitle>Swezey and others, 2013</resAltTitle><date><pubDate>2017-01-20</pubDate></date><citRespParty><rpOrgName>Cambridge University Press (CUP)</rpOrgName><rpCntInfo><cntAddress><delPoint>n/a</delPoint></cntAddress></rpCntInfo><role><RoleCd value="010"/></role></citRespParty><citRespParty><rpOrgName>Arthur P. Schultz</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>John P. McGeehin</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher P. Garrity</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Wilma AlemÃ¡n GonzÃ¡lez</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher S. Swezey</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher E. Bernhardt</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Shannon A. Mahan</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>William R. Doar</rpOrgName><role><RoleCd value="006"/></role></citRespParty><presForm><fgdcGeoform>publication</fgdcGeoform></presForm><datasetSeries><seriesName>Quaternary Research</seriesName><issId>v. 80, no. 02</issId></datasetSeries><otherCitDet>Swezey, C.S., Schultz, A.P., AlemÃ¡n GonzÃ¡lez, W.B., Bernhardt, C.E., Doar, W.R., III, Garrity, C.P., Mahan, S.A., and McGeehin, J.P., 2013, Quaternary eolian dunes in the Savannah River Valley, Jasper County, South Carolina, USA: Quaternary Research, v. 80, no. 2, p. 250â€“264. [Also available at http://www.sciencedirect.com/science/article/pii/S0033589413000719.]</otherCitDet><citOnlineRes><linkage>http://dx.doi.org/10.1016/j.yqres.2013.06.007</linkage></citOnlineRes></srcCitatn><srcExt><exDesc>publication date</exDesc><tempEle><TempExtent><exTemp><TM_Instant><tmPosition>2017-01-01</tmPosition></TM_Instant></exTemp></TempExtent></tempEle></srcExt></dataSource></dataLineage></dqInfo><spatRepInfo><VectSpatRep><geometObjs Name="SurficialPolygons"><geoObjTyp><GeoObjTypCd value="002" Sync="TRUE"></GeoObjTypCd></geoObjTyp><geoObjCnt Sync="TRUE">695</geoObjCnt></geometObjs><topLvl><TopoLevCd value="001" Sync="TRUE"></TopoLevCd></topLvl></VectSpatRep></spatRepInfo><eainfo><detailed Name="SurficialPolygons"><enttyp><enttypl>Attribute Table</enttypl><enttypd>Table containing attribute information associated with the data set.</enttypd><enttypds>Producer defined</enttypds><enttypt Sync="TRUE">Feature Class</enttypt><enttypc Sync="TRUE">695</enttypc></enttyp><attr><attrlabl Sync="TRUE">OBJECTID</attrlabl><attalias Sync="TRUE">OBJECTID</attalias><attrtype Sync="TRUE">OID</attrtype><attwidth Sync="TRUE">4</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale><attrdef Sync="TRUE">Internal feature number.</attrdef><attrdefs Sync="TRUE">Esri</attrdefs><attrdomv><udom Sync="TRUE">Sequential unique whole numbers that are automatically generated.</udom></attrdomv></attr><attr><attrlabl Sync="TRUE">SHAPE</attrlabl><attalias Sync="TRUE">SHAPE</attalias><attrtype Sync="TRUE">Geometry</attrtype><attwidth Sync="TRUE">0</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale><attrdef Sync="TRUE">Feature geometry.</attrdef><attrdefs Sync="TRUE">Esri</attrdefs><attrdomv><udom Sync="TRUE">Coordinates defining the features.</udom></attrdomv></attr><attr><attrlabl>MapUnit</attrlabl><attrdef>Short plain-text identifier of the map unit.</attrdef><attrdefs>Producer defined</attrdefs><attrdomv><edom><edomv>Qs3</edomv><edomvd>Sand terraces within the Savannah River flood plain (Quaternary)â€”0.5- to 2-m (1.6- to 6.6-ft)-thick, pale-yellowish-orange (10YR 8/4) and light-gray (N8) sand, silt, and clay. Sand grains are fine to coarse grained and are composed of quartz (99 percent) and rock fragments (1 percent) that include mica and garnet. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. Terraces Qt3 to Qt5 within the Savannah River flood plain are formed on this unit. These sediments are thought to be Quaternary in age, spanning a time that ranges from older than the Qs1 sand hills (eolian dunes) to coeval with the sand hills. Eolian sand (Qs1) covers terrace Qt1 and older terraces to the east (Qt2 to Qt5), suggesting that these terraces are older than the eolian sand. However, one sample of sand (GAW-37; table 1) collected from a depth of 183 centimeters (cm) below the surface of terrace Qt4 yielded a preferred OSL age of 108.0Â±12.0 ka, which is much older than most of the preferred OSL ages that range from approximately 33 to 19 ka (table 1) from the sand hills of Qs1. Other OSL ages from the terraces are coeval with the OSL ages from the sand hills. For example, (1) a sample of sandy mud (GAW-29; table 1) collected from a depth of 61 cm below the surface of terrace Qt5 yielded a preferred OSL age of 39.7Â±3.6 ka, (2) a sample of sand (GAW-14; table 1) collected from a depth of 70 cm below the surface of terrace Qt4 yielded a preferred OSL age of 24.2Â±1.2 ka, and (3) a sample of sandy mud (GAW-28; table 1) collected from a depth of 84 cm below the surface of terrace Qt4 yielded a preferred OSL age 23.6Â±2.1 ka. Unit Qs3 is interpreted as fluvial terrace deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm3</edomv><edomvd>Sand and mud in abandoned channels (Quaternary)â€”0.3- to 10.7-m (1- to 35-ft)-thick, yellowish-orange (10YR 8/4) and light-gray (N7) sand, silt, and clay in abandoned channels on the west side of the high terrace that forms the eastern border of the Savannah River flood plain where the elevation changes abruptly from approximately 10 to &gt;15 m above sea level. This unit is mapped as deposits associated with the following two geomorphic features: (1) relict meandering channels (Qsm3), and (2) extra-channel areas that are adjacent to but outside of a channel (Qsm4). Sand grains are very fine to coarse grained and are composed of quartz (99 percent) and rock fragments (1 percent) that include mica, garnet, and epidote. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. Units Qsm3 and Qsm4 are interpreted as channel and point-bar deposits of a relict meandering fluvial system that is older than the modern Savannah River flood plain. The sizes of the relict meandering channels are similar to those of the modern Savannah River, suggesting similar flow regimes. It is presumed that the sand and mud in these relict channels are Quaternary in age</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qgsm</edomv><edomvd>Gravel, sand, and mud (Pleistocene)â€”3.0- to 9.1-m (10- to 30-ft)-thick, sand and gravelly sand that fines upward to sand and then muddy sand. The lower part (sand and gravelly sand) is very light gray (N8) to medium gray (N5), whereas the upper part is mottled light-brown (5YR 5/6), pale-brown (5YR 5/2), yellowish-orange (10YR 4/6), yellowish-gray (5YR 7/2), and moderate-greenish-yellow (10Y 7/4) muddy sand. Gravel in the lower part is granules and pebbles of quartz and feldspar. Sand grains in the lower part are fine to very coarse grained and are composed of quartz (98 percent) and rock fragments (2 percent) that include mica, garnet, epidote, and amphibole. Sand grains in the upper part are very fine to fine grained and are composed of quartz (98 percent) and rock fragments (2 percent) that include mica and opaque minerals. The lower part of the unit is poorly to moderately sorted, whereas the upper part of the unit is moderately sorted to well sorted. Primary sedimentary structures are not apparent. Unit Qgsm forms an overall fining-upward sequence and is interpreted as a fluvial deposit. A terrace is formed on this unit in the southeasternmost part of the study area and appears to be greatly weathered. On the basis of elevation and geomorphological expression in the light detection and ranging (lidar) image (map B), the unit is thought to be older than terraces Qt1 through Qt5</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm5</edomv><edomvd>Sand and mud (Pleistocene)â€”0.3- to 9.1-m (1- to 30-ft)-thick, medium-light-gray (N6) to light-gray (N7) sand and muddy sand. Sand grains are fine to coarse grained and are composed predominantly of quartz. The unit is poorly to well sorted. Primary sedimentary structures are not apparent. The unit forms alluvial fans of sediment where abandoned fluvial channels enter the east side of the Savannah River valley. Unit Qsm5 is interpreted as alluvial and fluvial sediments</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsmp4</edomv><edomvd>Sand, mud, and peat in fluvial channels (Quaternary)â€”0.3- to 3.7-m (1- to 12-ft)-thick, light-gray (N7) to medium-bluish-gray (5B 5/1) to brownish-gray (5YR 4/1) to black (N1) sand, mud, and peat in abandoned fluvial channels truncated by the westernmost terrace (Qt0) on the Savannah River flood plain. Sand grains are very fine to very coarse grained and are composed primarily of quartz. The unit is well to very well sorted. Primary sedimentary structures are not apparent. The unit is found in abandoned channels on terraces Qt1 through Qt5 shown on maps A and B. A sample of wood (WW8888; fig. 4) from this unit in gouge core C1 yielded a radiocarbon age of 41,890Â±930 14C yr BP (46,841 to 43,856 cal yr BP) (table 3). This age approaches the older limit for radiocarbon dating, and thus may be a minimum age for the sample (and a minimum age for the channel). This channel is younger than the terraces into which it has incised. Unit Qsmp4 is interpreted as fluvial and swamp deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qs2</edomv><edomvd>Sand (Quaternary)â€”0.3- to 9.1-m (1- to 30-ft)-thick, yellowish-orange (10YR 8/4) and light-gray (N7) sand. Sand grains are fine to very coarse grained and are composed of quartz (99 percent) and rock fragments (1 percent) that include mica, garnet, and epidote. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. The unit forms irregular ridges between channels. The ridges (and channels) are on (or in) terraces Qt1 through Qt5 that are bounded on the west by low-relief escarpments that trend northwest.</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm1</edomv><edomvd>Sand and mud (Holocene)â€”0.3- to 4.6-m (1- to 15-ft)-thick, white (N9) to medium-gray (N5) sand, silt, and clay. Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. The unit is found on the youngest terrace (westernmost terrace) of the Savannah River (terrace Qt0 on maps A and B) between the Savannah River and the eolian dunes (Qs1), and in most locations unit Qsm1 is associated with unit Qsm2. Unit Qsm1 is interpreted as fluvial channel point-bar deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qs1</edomv><edomvd>Sand (Quaternary)â€”0.3- to 9.1-m (1- to 30-ft)-thick, yellowish-orange (10YR 6/6) sand, overlain by a 0.1- to 0.6-m-thick veneer of brown (10YR 6/2) sand with iron-oxide coating. Sand grains are mostly fine to medium grained and are composed of quartz (99 percent) and rock fragments (1 percent) that include mica and opaque minerals; feldspar is notably absent. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. This unit forms a relatively continuous group of sand hills that are located at distances of 0 to 5 kilometers east of the modern river channel, and forms various isolated sand hills and ridges that are also located east of the modern river channel. Where discernible, the morphologies of individual hills range from parabolic shapes (with tails pointing west) to isolated circular and linear shapes. Samples from this unit have yielded 15 optically stimulated luminescence (OSL) ages (table 1). Using the preferred ages given in bold in table 1 and taking into account the reported ranges of uncertainty, 13 of these ages range from approximately 35.4 to 18.0 ka, and two of these ages range from approximately 11.0 to 9.5 ka (GAW-13 and GAW-11, table 1). The two younger ages are from relatively isolated sand hills and ridges. Unit Qs1 is interpreted as eolian dune deposits and is described in greater detail in Swezey and others (2013)</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Ngsm</edomv><edomvd>Gravel, sand, and mud (lower Pliocene?)â€”0.3-m to at least 17.4-m (1-ft to at least 57-ft)-thick, mottled light-gray (N7) and pale-reddish-brown (10R 5/4) to pale-yellowish-orange (10YR 8/6) sand and sandy mud, a few beds of gravelly sand, and a few beds of mud (silt and clay). Light-gray intervals are composed of sand (20 to 30 percent) and mud (70 to 80 percent), whereas pale-reddish-brown intervals are composed of sand (50 to 60 percent) and mud (40 to 50 percent). Most sand grains are fine to medium grained and are composed of quartz (99 percent) and rock fragments (1 percent) that include mica, garnet, and epidote. Individual beds range from poorly to moderately to well sorted. Primary sedimentary structures are not apparent at most locations, although crossbedding is visible in a few beds at one outcrop on the Savannah River. This unit, which is visible at one outcrop along the Savannah River (photographs 1 and 2), was encountered in drill core C2 and auger cores (figs. 2 and 3), and forms a high terrace that demarks the east side of the Savannah River valley. Relict meandering channels and extra-channel areas (mapped separately as Qsm3 and Qsm4) are present on the west side of this high terrace. Unit Ngsm was mapped by Doar (2008) as the Pleistocene Ladson Formation, and was mapped by Doar (2013b) as the Pleistocene Penholoway Formation. The unit is similar in both appearance and stratigraphic position to strata that are mapped collectively in Georgia as the Pliocene Cypresshead Formation (Huddlestun, 1988). Unit Ngsm is interpreted as estuarine to marginal marine sediments and beach ridges</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm4</edomv><edomvd>Sand and mud in abandoned channels (Quaternary)â€”0.3- to 10.7-m (1- to 35-ft)-thick, yellowish-orange (10YR 8/4) and light-gray (N7) sand, silt, and clay in abandoned channels on the west side of the high terrace that forms the eastern border of the Savannah River flood plain where the elevation changes abruptly from approximately 10 to &gt;15 m above sea level. This unit is mapped as deposits associated with the following two geomorphic features: (1) relict meandering channels (Qsm3), and (2) extra-channel areas that are adjacent to but outside of a channel (Qsm4). Sand grains are very fine to coarse grained and are composed of quartz (99 percent) and rock fragments (1 percent) that include mica, garnet, and epidote. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. Units Qsm3 and Qsm4 are interpreted as channel and point-bar deposits of a relict meandering fluvial system that is older than the modern Savannah River flood plain. The sizes of the relict meandering channels are similar to those of the modern Savannah River, suggesting similar flow regimes. It is presumed that the sand and mud in these relict channels are Quaternary in age</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsmp3</edomv><edomvd>Sand, mud, and peat (Quaternary)â€”0.3- to 12.2-m (1- to 40-ft)-thick, light-gray (N7) to black (N1) sand, silt, clay, and peat. Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is well to very well sorted. Primary sedimentary structures include laminations, at some locations. The unit is found in areas of low elevation and poor drainage, and rests on a series of low-relief terraces (Qt1 through Qt5). Unit Qsmp3 is interpreted as fluvial, swamp, and marsh deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsm2</edomv><edomvd>Sand and mud (Holocene)â€”Two units are mapped together and are described below as unit 1 and unit 2. Both units are found on the youngest terrace (westernmost terrace) of the Savannah River (terrace Qt0 on maps A and B) Unit 1: 0.3- to 1.5-m (1- to 5-ft)-thick, white (N9) to light-yellowish- orange (10YR 8/6) sand and mud. Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. The unit forms low ridges adjacent to river channels. As described in Swezey and others (2013), this unit occurs west of and truncates the youngest eolian dunes (Qs1), which are dated at approximately 10 ka (kilo-annum, or thousand years before present). Unit 1 of Qsm2 is interpreted as levee deposits Unit 2: 0.3- to 2.1-m (1- to 7-ft)-thick, dark-yellowish-brown (10YR 4/2), brown (10Y 6/6), moderate-yellowish-orange (10YR 6/6), dark-gray (N3), and light-gray (N7) sand and mud. Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is moderately to well sorted. Primary sedimentary structures are not apparent. The unit is found along the sides of small drainages that have breached levee deposits of the Savannah River. This unit occurs west of and truncates the youngest eolian dunes (Qs1), which are dated at approximately 10 ka (Swezey and others, 2013). Unit 2 of Qsm2 is interpreted as crevasse splay deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Nsm</edomv><edomvd>Sand and mud, with phosphate grains (lower Miocene)â€”At least 15.5-m (51-ft)-thick, light-olive-gray (5Y 5/2) to yellowish-gray (5Y 7/2) to grayish-olive (10Y 4/2) clay, silt, sand, and muddy sand. Sand grains are very fine to fine grained and are composed of quartz (80 to 95 percent) and phosphate (5 to 20 percent). Laminations are visible in some beds. The unit is not exposed in outcrop, but was encountered in drill core C2 and auger cores (figs. 2 and 3). The early Miocene age of this unit is constrained by biostratigraphic data from sample R6709 A in drill core C2 (table 2). Unit Nsm is interpreted as shallow marine sediments</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsmp1</edomv><edomvd>Sand, mud, and peat (Holocene)â€”0.3- to 12-meters (m) (1- to 39-feet [ft])-thick, medium-light-gray (N6) to medium-bluish-gray (5B 5/1) to moderate-brown (5YR 3/4) to black (N1) sand, silt, clay, and peat in closed depressions among the sand hills (Qs1). Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is well to very well sorted. Primary sedimentary structures include laminations, in some places. Samples from this unit in vibracore C3 (on maps A and B; fig. 4) from a closed depression yielded radiocarbon ages ranging from 8,275Â±30 14C yr BP (9,403 to 9,135 cal yr BP) to modern. Additional details about this drill core may be found in Bernhardt and others (2012). Unit Qsmp1 is interpreted as interdune swamp deposits</edomvd><edomvds>Producer defined</edomvds></edom><edom><edomv>Qsmp2</edomv><edomvd>Sand, mud, and peat (Holocene)â€”0.3- to 1.8-m (1- to 6-ft)-thick, light-gray (N7) to black (N1) sand, silt, clay, and peat in abandoned fluvial channels on the westernmost terrace of the Savannah River (terrace Qt0 on maps A and B). Sand grains are very fine to medium grained and are composed predominantly of quartz. The unit is well to very well sorted. Primary sedimentary structures are not apparent. Unit Qsmp2 is interpreted as alluvial or swamp deposits that accumulated in abandoned fluvial channels</edomvd><edomvds>Producer defined</edomvds></edom></attrdomv><attalias Sync="TRUE">MapUnit</attalias><attrtype Sync="TRUE">String</attrtype><attwidth Sync="TRUE">10</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr><attr><attrlabl>SHAPE_Area</attrlabl><attrdef>Area of feature in internal units squared.</attrdef><attrdefs>ESRI</attrdefs><attrdomv><rdom><rdommin>16.7387930713137</rdommin><rdommax>33518221.7252577</rdommax></rdom><udom Sync="TRUE">Positive real numbers that are automatically generated.</udom></attrdomv><attalias Sync="TRUE">SHAPE_Area</attalias><attrtype Sync="TRUE">Double</attrtype><attwidth Sync="TRUE">8</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr><attr><attrlabl>SHAPE_Length</attrlabl><attrdef>Length of feature in internal units.</attrdef><attrdefs>ESRI</attrdefs><attrdomv><rdom><rdommin>15.0048870911479</rdommin><rdommax>284191.070173028</rdommax><attrunit>meter</attrunit></rdom><udom Sync="TRUE">Positive real numbers that are automatically generated.</udom></attrdomv><attalias Sync="TRUE">SHAPE_Length</attalias><attrtype Sync="TRUE">Double</attrtype><attwidth Sync="TRUE">8</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr><attr><attrlabl>mapDesc</attrlabl><attrdef>Defines and describes geologic map units in the feature class.</attrdef><attrdefs>Producer defined</attrdefs><attrdomv><udom>Defines and describes geologic map units in the feature class. 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No fees are applicable for obtaining the data set.</resFees></distorOrdPrc><distorFormat><formatName>Digital Data</formatName></distorFormat><distorTran><onLineSrc><linkage>https://doi.org/10.3133/sim3424</linkage></onLineSrc></distorTran></distributor><distTranOps><onLineSrc><linkage>https://pubs.er.usgs.gov/sim3424</linkage></onLineSrc><onLineSrc><linkage>https://doi.org/10.3133/sim3424</linkage></onLineSrc></distTranOps><distFormat><formatName Sync="TRUE">File Geodatabase Feature Class</formatName></distFormat></distInfo><dataIdInfo><idCitation><resTitle>Geology of the Hardeeville NW Quadrangle and Parts of the Brighton and Pineland Quadrangles, Jasper County, South Carolina</resTitle><date><pubDate>2019-02-11</pubDate></date><citRespParty><rpOrgName>Lucy E. Edwards</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>John P. McGeehin</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>William R. Doar III</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>U.S. Geological Survey</rpOrgName><rpCntInfo><cntAddress><delPoint>Reston, Virginia</delPoint></cntAddress></rpCntInfo><role><RoleCd value="010"/></role></citRespParty><citRespParty><rpOrgName>Christopher P. Garrity</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Arthur P. Schultz</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher E. Bernhardt</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>E. Allen Crider</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher S. Swezey</rpOrgName><role><RoleCd value="006"/></role></citRespParty><presForm><fgdcGeoform>Vector Digital Data Set (Polygon)</fgdcGeoform><PresFormCd value="005" Sync="TRUE"></PresFormCd></presForm><datasetSeries><seriesName>U.S. Geological Survey Scientific Investigations Map</seriesName><issId>3424</issId></datasetSeries></idCitation><idAbs>This publication portrays the geology of the Hardeeville NW quadrangle and parts of the Brighton and Pineland quadrangles that are within Jasper County, South Carolina. This study area is located in the Atlantic Coastal Plain province, approximately 50 to 70 kilometers (km) inland from the coast. The data are compiled from geological field mapping, light detection and ranging (lidar) elevation data, cores, optically stimulated luminescence (OSL) ages, radiocarbon ages, and biostratigraphic interpretations. Most of the study area is occupied by the valley of the Savannah River, and exposures of geologic units are very limited. Traditional geologic mapping in this area is difficult because of limited access, subdued topography, extensive swamps, and abundant vegetation.</idAbs><idPurp>The purpose of this information is to provide primary data for basic and applied earth-science investigations by producing geologic maps that contribute to a comprehensive nation-wide program of geologic mapping of bedrock and surface deposits.</idPurp><idCredit>Please acknowledge U.S. Geological Survey as the source of the data.</idCredit><idStatus><ProgCd value="001"/></idStatus><idPoC><rpIndName>Christopher Swezey</rpIndName><rpOrgName>U.S. Geological Survey, Northeast Region</rpOrgName><rpPosName>Research Geologist</rpPosName><rpCntInfo><cntPhone><voiceNum>703-648-6444</voiceNum><faxNum>703-648-6953</faxNum></cntPhone><cntAddress addressType="postal"><delPoint>Mail Stop 926A, 12201 Sunrise Valley Dr</delPoint><city>Reston</city><adminArea>VA</adminArea><postCode>20192</postCode><country>US</country><eMailAdd>cswezey@usgs.gov</eMailAdd></cntAddress></rpCntInfo><role><RoleCd value="007"/></role></idPoC><resMaint><maintFreq><MaintFreqCd value="011"/></maintFreq></resMaint><placeKeys><keyword>Pineville</keyword><keyword>Brighton</keyword><keyword>Jasper</keyword><keyword>United States</keyword><keyword>Hardeeville NW</keyword><keyword>South Carolina</keyword><thesaName><resTitle>Common geographic areas</resTitle></thesaName></placeKeys><themeKeys><keyword>geoscientificInformation</keyword><thesaName><resTitle>ISO 19115 Topic Category</resTitle></thesaName></themeKeys><themeKeys><keyword>geologic time periods</keyword><keyword>Pliocene</keyword><keyword>Holocene</keyword><keyword>geologic contacts</keyword><keyword>geologic maps</keyword><keyword>Quaternary</keyword><keyword>Miocene</keyword><keyword>surficial geologic units</keyword><thesaName><resTitle>USGS Thesaurus</resTitle></thesaName></themeKeys><themeKeys><keyword>Sand</keyword><keyword>Gravel</keyword><keyword>Eolian material</keyword><keyword>Clay or mud</keyword><keyword>Peat</keyword><keyword>Terrace</keyword><thesaName><resTitle>Lithologic classification of geologic map units</resTitle></thesaName></themeKeys><searchKeys><keyword>geologic time periods</keyword><keyword>Sand</keyword><keyword>Pliocene</keyword><keyword>Holocene</keyword><keyword>Pineville</keyword><keyword>Brighton</keyword><keyword>geologic contacts</keyword><keyword>Gravel</keyword><keyword>geologic maps</keyword><keyword>geoscientificInformation</keyword><keyword>Jasper</keyword><keyword>Eolian material</keyword><keyword>United States</keyword><keyword>Hardeeville NW</keyword><keyword>Clay or mud</keyword><keyword>Peat</keyword><keyword>Quaternary</keyword><keyword>Miocene</keyword><keyword>Terrace</keyword><keyword>South Carolina</keyword><keyword>surficial geologic units</keyword></searchKeys><resConst><LegConsts><useLimit>Although all data and software released have been used by the USGS, no warranty, expressed or implied, is made by the USGS as to the accuracy of the data and related materials and (or) the functioning of the software.</useLimit><othConsts>None. Please see 'Distribution Info' for details.</othConsts></LegConsts></resConst><resConst><Consts><useLimit>Unless otherwise stated, all data, metadata and related materials are considered to satisfy the quality standards relative to the purpose for which the data were collected. Although these data and associated metadata have been reviewed for accuracy and completeness and approved for release by the U.S. Geological Survey (USGS), no warranty expressed or implied is made regarding the display or utility of the data on any other system or for general or scientific purposes, nor shall the act of distribution constitute any such warranty. Users of this geospatial data and geologic information derived there from should acknowledge the U.S. Geological Survey as the source of the data. Although software enables a user to display images at various scales, map data in this report should not be used at scales greater than 1:24,000.</useLimit></Consts></resConst><spatRpType><SpatRepTypCd value="001"/></spatRpType><dataLang><languageCode value="eng"/><countryCode value="USA" Sync="TRUE"></countryCode></dataLang><tpCat><TopicCatCd value="008"/></tpCat><envirDesc>Environment as of Metadata Creation: Microsoft Windows 7 Version 6.1 (Build 7601) Service Pack 1; Esri ArcGIS 10.6 (Build 8321) Service Pack N/A (Build N/A)</envirDesc><dataExt><exDesc>publication date</exDesc><tempEle><TempExtent><exTemp><TM_Period><tmBegin>2009-12-01</tmBegin><tmEnd>2019-02-11</tmEnd></TM_Period></exTemp></TempExtent></tempEle><geoEle/></dataExt><dataExt><geoEle><GeoBndBox><westBL>-81.2791</westBL><eastBL>-81.1289</eastBL><southBL>32.4237</southBL><northBL>32.556</northBL></GeoBndBox></geoEle></dataExt><suppInfo>This feature class contains geologic unit boundaries for the Hardeeville NW quadrangle and parts of the Brighton and Pineland quadrangles, Jasper County, South Carolina. Digital data were compiled from source data at a scale of 1:24,000 and are not intended to be used at a larger (greater detail) scale. The release of these data will allow the general public, academia, and earth science professional to view and evaluate geologic data at the 1:24,000 scale. It is hoped that the use of these data, either by themselves or in relation to other data, may lead to new interpretations of the geology of the mapped area.</suppInfo><dataExt><geoEle><GeoBndBox esriExtentType="search"><exTypeCode Sync="TRUE">1</exTypeCode><westBL Sync="TRUE">-81.279060</westBL><eastBL Sync="TRUE">-81.128880</eastBL><northBL Sync="TRUE">32.555970</northBL><southBL Sync="TRUE">32.423730</southBL></GeoBndBox></geoEle></dataExt></dataIdInfo><dqInfo><dqScope><scpLvl><ScopeCd value="005"/></scpLvl></dqScope><report type="DQTopConsis"><evalMethDesc>Topological accuracy was tested using topology validation tools. Specific errors that were checked included: Polygon overlaps and gaps, coincident contact lines and geologic unit borders, self overlapping lines and superfluous pseudo nodes. No duplicate features exist nor duplicate points in a data string. Intersecting lines are separated into individual line segments at the point of intersection. Feature classes in the geodatabase are topologically clean.</evalMethDesc></report><report type="DQConcConsis"><measDesc>Topological accuracy was tested using topology validation tools. Specific errors that were checked included: Polygon overlaps and gaps, coincident contact lines and geologic unit borders, self overlapping lines and superfluous pseudo nodes. No duplicate features exist nor duplicate points in a data string. Intersecting lines are separated into individual line segments at the point of intersection. Feature classes in the geodatabase are topologically clean.</measDesc></report><report type="DQCompOm"><measDesc>Data set complete. No data was intentionally omitted from the source map.</measDesc></report><report type="DQQuanAttAcc"><measDesc>Attribute accuracy was tested by manual comparison of the source with hard copy printouts and/or symbolized display of the digital geologic data on an interactive computer graphic system. In addition, attributes were compared to a master set of valid geologic unit attributes.</measDesc></report><report type="DQAbsExtPosAcc" dimension="horizontal"><measDesc>A formal accuracy assessment of the horizontal positional information in the data set has not been conducted.</measDesc></report><report type="DQAbsExtPosAcc" dimension="vertical"><measDesc>A formal accuracy assessment of the vertical positional information in the data set has either not been conducted, or is not applicable.</measDesc></report><dataLineage><prcStep><stepDesc>Christopher Swezey and Arthur Schultz obtained previously published topographic maps and previously published geologic maps of the area (Doar, 2008, 2013a, 2013b).</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Crider registered and rectified the mylar over the LiDAR hillshade in ArcGIS. Schultz directly digitized the linework onscreen, using a hillshade and slope DEM from the LiDAR DEM and the registered mylar.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Swezey and Schultz field-checked the various geomorphological features that were visible in the LiDAR imagery, paying particular attention to boundaries of the geomorphologic features.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Crider took linework, smoothed it, and made sure that the linework was topologically clean and located properly. Swezey reviewed the resulting product, and made some modifications after checking against the field data obtained by Swezey and Schultz.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Swezey and Schultz dug pits into these features and noted sediment composition, noted changes in vegetation assemblages associated with some of the features, and collected sediment samples for OSL dating. Swezey and Schultz also compared the sediments found in their pits with USDA soil maps of Jasper County (Stuck, 1980). Swezey and Schultz also drilled cores in the field area in order to verify vertical stratigraphic contacts.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>Swezey and Schultz obtained LiDAR imagery of the Hardeeville NW quadrangle and the southern half of the Brighton and Pineland quadrangles.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>LiDAR imagery of the field area was processed by Garrity, and field data were collected by Swezey and Schultz. Schultz placed mylar on top of the LiDAR plot, consulted with field data obtained by Swezey and Schultz, and traced over features of the hillshade.</stepDesc><stepDateTm date="unknown"/></prcStep><prcStep><stepDesc>The LiDAR was processed by Christopher Garrity. The LiDAR imagery revealed low-relief geomorphological features that were not apparent in the previously published maps.</stepDesc><stepDateTm date="unknown"/></prcStep><dataSource><srcDesc>This citation was used in the production of this database, either in the description of map units, or the production of geologic polygons, contacts and faults, or the additional supporting structural and cartographic information.</srcDesc><srcMedName><MedNameCd value="018"/></srcMedName><srcCitatn><resTitle>Quaternary eolian dunes in the Savannah River Valley, Jasper County, South Carolina, USA</resTitle><resAltTitle>Swezey and others, 2013</resAltTitle><date><pubDate>2017-01-20</pubDate></date><citRespParty><rpOrgName>Wilma AlemÃ¡n GonzÃ¡lez</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Shannon A. Mahan</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Cambridge University Press (CUP)</rpOrgName><rpCntInfo><cntAddress><delPoint>n/a</delPoint></cntAddress></rpCntInfo><role><RoleCd value="010"/></role></citRespParty><citRespParty><rpOrgName>Christopher P. Garrity</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Arthur P. Schultz</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>William R. Doar</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>John P. McGeehin</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher S. Swezey</rpOrgName><role><RoleCd value="006"/></role></citRespParty><citRespParty><rpOrgName>Christopher E. Bernhardt</rpOrgName><role><RoleCd value="006"/></role></citRespParty><presForm><fgdcGeoform>publication</fgdcGeoform></presForm><datasetSeries><seriesName>Quaternary Research</seriesName><issId>v. 80, no. 02</issId></datasetSeries><otherCitDet>Swezey, C.S., Schultz, A.P., AlemÃ¡n GonzÃ¡lez, W.B., Bernhardt, C.E., Doar, W.R., III, Garrity, C.P., Mahan, S.A., and McGeehin, J.P., 2013, Quaternary eolian dunes in the Savannah River Valley, Jasper County, South Carolina, USA: Quaternary Research, v. 80, no. 2, p. 250â€“264. [Also available at http://www.sciencedirect.com/science/article/pii/S0033589413000719.]</otherCitDet><citOnlineRes><linkage>http://dx.doi.org/10.1016/j.yqres.2013.06.007</linkage></citOnlineRes></srcCitatn><srcExt><exDesc>publication date</exDesc><tempEle><TempExtent><exTemp><TM_Instant><tmPosition>2017-01-01</tmPosition></TM_Instant></exTemp></TempExtent></tempEle></srcExt></dataSource></dataLineage></dqInfo><spatRepInfo><VectSpatRep><geometObjs Name="GeochronPoints"><geoObjTyp><GeoObjTypCd value="004" Sync="TRUE"></GeoObjTypCd></geoObjTyp><geoObjCnt Sync="TRUE">20</geoObjCnt></geometObjs><topLvl><TopoLevCd value="001" Sync="TRUE"></TopoLevCd></topLvl></VectSpatRep></spatRepInfo><eainfo><detailed Name="GeochronPoints"><enttyp><enttypl>Attribute Table</enttypl><enttypd>Table containing attribute information associated with the data set.</enttypd><enttypds>Producer defined</enttypds><enttypt Sync="TRUE">Feature Class</enttypt><enttypc Sync="TRUE">20</enttypc></enttyp><attr><attrlabl>Latitude</attrlabl><attrdef>Latitude</attrdef><attalias Sync="TRUE">Latitude</attalias><attrtype Sync="TRUE">Double</attrtype><attwidth Sync="TRUE">8</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr><attr><attrlabl>AgeDetermination</attrlabl><attrdef>Date the age of the sample was determined</attrdef><attalias Sync="TRUE">AgeDetermination</attalias><attrtype Sync="TRUE">Double</attrtype><attwidth Sync="TRUE">8</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr><attr><attrlabl>OSLSample</attrlabl><attrdef>OSL Sample ID</attrdef><attalias Sync="TRUE">OSLSample</attalias><attrtype Sync="TRUE">String</attrtype><attwidth Sync="TRUE">254</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr><attr><attrlabl>OBJECTID</attrlabl><attrdef>Internal feature number.</attrdef><attrdefs>Esri</attrdefs><attrdomv><udom>Sequential unique whole numbers that are automatically generated.</udom></attrdomv><attalias Sync="TRUE">OBJECTID</attalias><attrtype Sync="TRUE">OID</attrtype><attwidth Sync="TRUE">4</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr><attr><attrlabl>Longitude</attrlabl><attrdef>Longitude</attrdef><attalias Sync="TRUE">Longitude</attalias><attrtype Sync="TRUE">Double</attrtype><attwidth Sync="TRUE">8</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr><attr><attrlabl>Shape</attrlabl><attrdef>Feature geometry.</attrdef><attrdefs>Esri</attrdefs><attrdomv><udom>Coordinates defining the features.</udom></attrdomv><attalias Sync="TRUE">Shape</attalias><attrtype Sync="TRUE">Geometry</attrtype><attwidth Sync="TRUE">0</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr><attr><attrlabl>AgeKa</attrlabl><attrdef>Age in thousands of years ago before present.</attrdef><attalias Sync="TRUE">AgeKa</attalias><attrtype Sync="TRUE">String</attrtype><attwidth Sync="TRUE">254</attwidth><atprecis Sync="TRUE">0</atprecis><attscale Sync="TRUE">0</attscale></attr></detailed><overview><eaover>The entity and attribute information provided here describes the tabular data associated with the data set. Please review the detailed descriptions that are provided (the individual attribute descriptions) for information on the values that appear as fields/table entries of the data set.</eaover><eadetcit>The entity and attribute information was generated by the individual and (or) agency identified as the originator of the data set. Please review the rest of the metadata record for additional details and information.</eadetcit></overview></eainfo><mdHrLvName Sync="TRUE">dataset</mdHrLvName><refSysInfo><RefSystem><refSysID><identCode code="4269" Sync="TRUE"></identCode><idCodeSpace Sync="TRUE">EPSG</idCodeSpace><idVersion Sync="TRUE">6.12(3.0.1)</idVersion></refSysID></RefSystem></refSysInfo><spdoinfo><ptvctinf><esriterm Name="GeochronPoints"><efeatyp Sync="TRUE">Simple</efeatyp><efeageom code="1" Sync="TRUE"></efeageom><esritopo Sync="TRUE">FALSE</esritopo><efeacnt Sync="TRUE">20</efeacnt><spindex Sync="TRUE">TRUE</spindex><linrefer Sync="TRUE">FALSE</linrefer></esriterm></ptvctinf></spdoinfo></metadata>����