<?xml version="1.0" encoding="UTF-8"?>
<?xml-stylesheet type="text/xsl" href="fgdc_classic.xsl"?>
<metadata xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:noNamespaceSchemaLocation="http://water.usgs.gov/GIS/metadata/usgswrd/fgdc-std-001-1998.xsd">
<idinfo>
<citation>
<citeinfo>
<origin>V.L. McGuire</origin>
<origin>S.M. Peterson</origin>
<pubdate>2008</pubdate>
<title>Digitial map of geologic units forming the base of the principal aquifer and areas where the base of aquifer is not well defined, Elkhorn-Loup Model area, north-central Nebraska</title>
<edition>(Version 1.0, March 04, 2008)</edition>
<geoform>vector digital data</geoform>
<serinfo>
<sername>U.S. Geological Survey Scientific Investigations Map</sername>
<issue>3042</issue>
</serinfo>
<pubinfo>
<pubplace>Reston, Va</pubplace>
<publish>U.S. Geological Survey</publish>
</pubinfo>
<onlink>http://water.usgs.gov/lookup/getspatial?sim3042_gu</onlink>
<lworkcit>
<citeinfo>
<origin>V.L. McGuire</origin>
<origin>S.M. Peterson</origin>
<pubdate>2008</pubdate>
<title>Base of Principal Aquifer for the Elkhorn-Loup Model Area, North-Central Nebraska</title>
<geoform>PDF document</geoform>
<serinfo>
<sername>U.S. Geological Survey Scientific Investigations Map</sername>
<issue>3042</issue>
</serinfo>
<pubinfo>
<pubplace>Reston, Va</pubplace>
<publish>U.S. Geological Survey</publish>
</pubinfo>
<onlink>http://pubs.usgs.gov/sim/3042/</onlink>
</citeinfo>
</lworkcit>
</citeinfo>
</citation>
<descript>
<abstract>The U.S. Geological Survey (USGS), in cooperation with the Lewis and Clark Natural Resources District (NRD), Lower Elkhorn NRD, Lower Loup NRD, Lower Platte North NRD, Lower Niobrara NRD, Middle Niobrara NRD, Upper Elkhorn NRD, and Upper Loup NRD, have agreed to cooperatively study water resources from prior to the beginning of irrigation development to 2005 in the Elkhorn-Loup Model (ELM) area using a ground-water-flow model.  The ELM area covers approximately 30,800 square miles, and extends from the Niobrara River in the north to the Platte River in the south.  The western boundary of the ELM area coincides with the western boundary of the Middle Niobrara, Twin Platte, and Upper Loup NRDs; the eastern boundary coincides with the approximate location of the westernmost extent of glacial till in eastern Nebraska. The initial ground-water-flow model was constructed with a single layer vertically to represent the aquifers of the Tertiary-age Ogallala Group and Quaternary-age alluvial deposits, with a uniform node spacing of 2 miles. The model will be calibrated to measured ground-water levels and estimated ground-water discharge to streams for the pre-ground-water development period (approximately 1940) and the simulation of the 1940-2005 period will be calibrated to measure ground-water level changes. The study results will assist Nebraska Department of Natural Resources and the NRDs in the ELM area to develop long-term strategies for managing hydrologically connected waters.

This dataset is one of three geospatial datasets that together revise previously published maps of the configuration of the base of the principal aquifer and of the geologic units that form the base of the principal aquifer in the study area; the revisions to the base-of-aquifer altitude are based on currently available or reinterpreted geologic logs of test holes and selected registered wells. The principal aquifer is the High Plains aquifer except in the northeast part of the model area, where the principal aquifer is an unnamed alluvial aquifer.

This dataset identifies and delimits approximately the extent of the geologic units forming the base of the principal aquifer and the areas where the base of principal aquifer surface is not well defined. Ambiguity in the calculated base of aquifer existed wherever this calculated base-of-aquifer altitude was above the mapped land surface. The calculated base of aquifer was above  the mapped land surface either because of inaccuracy in the mapped land surface or base of aquifer calculation or because the principal aquifer was thin or not present.</abstract>
<purpose>The purpose of this data release is to make available geospatial data that identity and delimit approximately the extent of the geologic units forming the base of the principal aquifer and the areas where the principal aquifer is not well defined in the Elkhorn-Loup Model area, north-central Nebraska. The dataset was produced in support of the Elkhorn-Loup Model.</purpose>
<supplinf>Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government.

Although this Federal Geographic Data Committee-compliant metadata file is intended to document the dataset in nonproprietary form, as well as in ArcGIS format, this metadata file may include some ArcGIS-specific terminology.</supplinf>
</descript>
<timeperd>
<timeinfo>
<sngdate>
<caldate>2008</caldate>
</sngdate>
</timeinfo>
<current>publication date</current>
</timeperd>
<status>
<progress>Complete</progress>
<update>As needed</update>
</status>
<spdom>
<bounding>
<westbc>
-102.128248</westbc>
<eastbc>
-97.274685</eastbc>
<northbc>
42.925235</northbc>
<southbc>
40.598895</southbc>
</bounding>
</spdom>
<keywords>
<theme>
<themekt>None</themekt>
<themekey>USGS</themekey>
<themekey>High Plains aquifer</themekey>
<themekey>Elkhorn-Loup Model Area</themekey>
<themekey>aquifer base</themekey>
<themekey>Ogallala aquifer</themekey>
</theme>
<theme>
<themekt>ISO 19115 Topic Category</themekt>
<themekey>inlandWaters</themekey>
<themekey>geoscientificInformation</themekey>
</theme>
<theme>
<themekt>Water Resources Thesaurus</themekt>
<themekey>Aquifer characteristics</themekey>
<themekey>Geohydrologic units</themekey>
</theme>
<place>
<placekt>None</placekt>
<placekey>Nebraska</placekey>
</place>
<stratum>
<stratkt>None</stratkt>
<stratkey>Brule Formation</stratkey>
<stratkey>White River Group</stratkey>
<stratkey>Upper Cretaceous</stratkey>
<stratkey>Lower Tertiary</stratkey>
<stratkey>Chadron Formation</stratkey>
<stratkey>Pierre Shale</stratkey>
<stratkey>Niobrara Formation</stratkey>
</stratum>
</keywords>
<accconst>none</accconst>
<useconst>This dataset is not intended to be used at scales larger than 1:350,000.</useconst>
<ptcontac>
<cntinfo>
<cntperp>
<cntper>McGuire, V.L.</cntper>
<cntorg>U.S. Geological Survey</cntorg>
</cntperp>
<cntpos>Hydrologist</cntpos>
<cntaddr>
<addrtype>mailing address</addrtype>
<address>5231 South 19th Street</address>
<city>Lincoln</city>
<state>NE</state>
<postal>68512</postal>
<country>USA</country>
</cntaddr>
<cntvoice>(402)328-4100</cntvoice>
<cntfax>(402)328-4101</cntfax>
<cntemail>Webmaster@ne20dnelnc.cr.usgs.gov</cntemail>
</cntinfo>
</ptcontac>
<browse>
<browsen>http://water.usgs.gov/GIS/browse/sim3042_gu.gif</browsen>
<browsed>Illustration of dataset.</browsed>
<browset>GIF</browset>
</browse>
<datacred>This dataset was prepared in cooperation with the Lewis and Clark Natural Resources District (NRD), Lower Elkhorn NRD, Lower Loup NRD, Lower Platte North NRD, Lower Niobrara NRD, Middle Niobrara NRD, Upper Elkhorn NRD, and Upper Loup NRD. 

The dataset was prepared using published datasets and reports by the Cooperative Hydrology Study, Nebraska Oil and Gas Commission, University of Nebraska-Lincoln, Conservation and Survey Division, and the U.S. Geological Survey and unpublished data in the test-hole files assembled by J.F. Ayers and maintained by the University of Nebraska-Lincoln, Conservation and Survey Division. 

E.D. Gutentag, U.S. Geological Survey (retired); J.B. Swinehart, University of Nebraska-Lincoln, Conservation and Survey Division; J.C. Cannia, U.S. Geological Survey; R.F. Diffendal, Jr., University of Nebraska-Lincoln, Conservation and Survey Division; and S.O. Lackey, University of Nebraska-Lincoln, Conservation and Survey Division, reviewed the report and provided valuable feedback. In addition, J.W. Goeke, University of Nebraska-Lincoln, Conservation and Survey Division, provided assistance interpreting the unpublished test-hole information and  R.M. Joeckel, University of Nebraska-Lincoln, Conservation and Survey Division, provided assistance with the test-hole data.</datacred>
<native>Microsoft Windows XP Version 5.1 (Build 2600) Service Pack 2; ESRI ArcCatalog 9.3.0.1770</native>
<crossref>
<citeinfo>
<origin>McGuire, V.L.</origin>
<origin>Peterson, S.M.</origin>
<pubdate>2009</pubdate>
<title>sim3042_tw--Digital map of the test-hole and well data used to estimate the configuration of the base of the principal aquifer and the geologic units underlying the principal aquifer in the Elkhorn-Loup model area, north-central Nebraska</title>
<geoform>vector digital data</geoform>
<serinfo>
<sername>U.S. Geological Survey Scientific Investigations Map</sername>
<issue>3042</issue>
</serinfo>
<pubinfo>
<pubplace>Reston, Va</pubplace>
<publish>U.S. Geological Survey</publish>
</pubinfo>
<onlink>http://water.usgs.gov/lookup/getspatial?sim3042_tw</onlink>
<lworkcit>
<citeinfo>
<origin>McGuire, V.L.</origin>
<origin>S.M. Peterson</origin>
<pubdate>2008</pubdate>
<title>Base of Principal Aquifer for the Elkhorn-Loup Model Area, North-Central Nebraska</title>
<geoform>pdf document</geoform>
<serinfo>
<sername>U.S. Geological Survey Scientific Investigations Map</sername>
<issue>3042</issue>
</serinfo>
<pubinfo>
<pubplace>Reston, Va</pubplace>
<publish>U.S. Geological Survey</publish>
</pubinfo>
<onlink>http://pubs.usgs.gov/sim/3042/</onlink>
</citeinfo>
</lworkcit>
</citeinfo>
</crossref>
<crossref>
<citeinfo>
<origin>McGuire, V.L.</origin>
<origin>Peterson, S.M.</origin>
<pubdate>2009</pubdate>
<title>sim3042_ab--Digital map of the configuration of the base of the principal aquifer in the Elkhorn-Loup Model area, north-central Nebraska</title>
<geoform>vector digital data</geoform>
<serinfo>
<sername>U.S. Geological Survey Scientific Investigations Map</sername>
<issue>3042</issue>
</serinfo>
<pubinfo>
<pubplace>Reston, Va</pubplace>
<publish>U.S. Geological Survey</publish>
</pubinfo>
<onlink>http://water.usgs.gov/lookup/getspatial?sim3042_ab</onlink>
<lworkcit>
<citeinfo>
<origin>McGuire, V.L.</origin>
<origin>Peterson, S.M.</origin>
<pubdate>2008</pubdate>
<title>Base of Principal Aquifer for the Elkhorn-Loup Model Area, North-Central Nebraska</title>
<geoform>pdf document</geoform>
<serinfo>
<sername>U.S. Geological Survey Scientific Investigations Map</sername>
<issue>3042</issue>
</serinfo>
<pubinfo>
<pubplace>Reston, Va</pubplace>
<publish>U.S. Geological Survey</publish>
</pubinfo>
<onlink>http://pubs.usgs.gov/sim/3042</onlink>
</citeinfo>
</lworkcit>
</citeinfo>
</crossref>
</idinfo>
<dataqual>
<attracc>
<attraccr>The mapped geologic units were compared to published reports, if available (see references listed in source information). The designations of the geologic unit that forms the base of the aquifer were reviewed by geologists familiar with the area--E.D. Gutentag, U.S. Geological Survey (retired); J.B. Swinehart, University of Nebraska-Lincoln, Conservation and Survey Division; J.C. Cannia, U.S. Geological Survey; R.F. Diffendal, Jr., University of Nebraska-Lincoln, Conservation and Survey Division; and S.O. Lackey, University of Nebraska-Lincoln, Conservation and Survey Division. Their feedback was incorporated into the report and the map.

The density of registered wells and test holes with data about the geologic unit that forms the base of aquifer varies greatly across the map area. The accuracy of the extent of geologic units that form the aquifer base in a given area is related directly to the density and availability of registered well and test-hole data with relevant information in that area. The approximate horizontal accuracy was derived by estimating the average distances between the registered wells and test holes in the vicinity of the geologic unit boundaries; this estimate is 3 miles.</attraccr>
</attracc>
<logic>Polygon topology is present.
The Arc Workstation Labelerrors command were used to verify that each polygon had one and only one label point.</logic>
<complete>The contacts of the geologic units that underlie the principal aquifer, and the areas where the base of the principal aquifer is not well defined, were based on the stratigraphic information from the test-hole lithologic and borehole geophysical logs as interpreted by the University of Nebraska-Lincoln, Conservation and Survey Division geologists and by the authors. These contacts are approximate, especially in areas where there are few test holes supporting the identity of the mapped geologic unit.</complete>
<posacc>
<horizpa>
<horizpar>Varies, typically within about 3 miles, but it depends on the density of applicable wells and test holes.</horizpar>
</horizpa>
<vertacc>
<vertaccr>Not applicable</vertaccr>
</vertacc>
</posacc>
<lineage>
<srcinfo>
<srccite>
<citeinfo>
<origin>Bentall, Ray</origin>
<origin>Dreeszen, V.H</origin>
<origin>Elder, J.A.</origin>
<origin>Jess, J.M.</origin>
<origin>Souders, V.L.</origin>
<origin>Birkel, W.H.</origin>
<origin>Braun, K.J.</origin>
<origin>Ellis, M.J.</origin>
<origin>Engel, G.B.</origin>
<origin>Engberg, R.A.</origin>
<origin>Shaffer, F.B.</origin>
<pubdate>1971</pubdate>
<title>Water Supplies and the land-the Elkhorn River Basin of Nebraska</title>
<geoform>document</geoform>
<serinfo>
<sername>Resource Atlas</sername>
<issue>No. 1</issue>
</serinfo>
<pubinfo>
<pubplace>Lincoln, Ne</pubplace>
<publish>University of Nebraska-Lincoln, Conservation and Survey Division</publish>
</pubinfo>
</citeinfo>
</srccite>
<srcscale>1000000</srcscale>
<typesrc>paper</typesrc>
<srctime>
<timeinfo>
<sngdate>
<caldate>unknown</caldate>
</sngdate>
</timeinfo>
<srccurr>publication date</srccurr>
</srctime>
<srccitea>Bentall and others, 1971</srccitea>
<srccontr>Geologic units in lower Elkhorn River Basin, Nebraska</srccontr>
</srcinfo>
<srcinfo>
<srccite>
<citeinfo>
<origin>Burchett, R.R.</origin>
<origin>Reed, E.C.</origin>
<origin>Dreeszen, V.H.</origin>
<origin>Prichard, G.E.</origin>
<pubdate>1975</pubdate>
<title>Bedrock geologic map showing thickness of overlying Quaternary deposits, Fremont quadrangle and part of the Omaha quadrangle, Nebraska</title>
<geoform>raster digital data</geoform>
<serinfo>
<sername>U.S. Geological Survey Miscellaneous Investigations Series</sername>
<issue>Map I-905</issue>
</serinfo>
<pubinfo>
<pubplace>Reston, Va</pubplace>
<publish>U.S. Geological Survey</publish>
</pubinfo>
<onlink>http://ngmdb.usgs.gov/Prodesc/proddesc_9487.htm</onlink>
</citeinfo>
</srccite>
<srcscale>250000</srcscale>
<typesrc>online and paper</typesrc>
<srctime>
<timeinfo>
<sngdate>
<caldate>unknown</caldate>
</sngdate>
</timeinfo>
<srccurr>publication date</srccurr>
</srctime>
<srccitea>Map I-905</srccitea>
<srccontr>Extent of bedrock units in the Fremont 1-degree by 2-degree quadrangle.</srccontr>
</srcinfo>
<srcinfo>
<srccite>
<citeinfo>
<origin>Burchett, R.R.</origin>
<origin>Dreeszen, V.H.</origin>
<origin>Souders, V.L.</origin>
<origin>Prichard, G.E.</origin>
<pubdate>1988</pubdate>
<title>Bedrock geologic map showing configuration of the bedrock surface in the Nebraska part of the Sioux City 1-degree x 2-degree quadrangle</title>
<geoform>raster digital data</geoform>
<serinfo>
<sername>U.S. Geological Survey Miscellaneous Investigations Series,</sername>
<issue>Map I-1879</issue>
</serinfo>
<pubinfo>
<pubplace>Reston, Va</pubplace>
<publish>U.S. Geological Survey</publish>
</pubinfo>
<onlink>http://ngmdb.usgs.gov/Prodesc/proddesc_9965.htm</onlink>
</citeinfo>
</srccite>
<srcscale>250000</srcscale>
<typesrc>online and paper</typesrc>
<srctime>
<timeinfo>
<sngdate>
<caldate>unknown</caldate>
</sngdate>
</timeinfo>
<srccurr>publication date</srccurr>
</srctime>
<srccitea>Map I-1879</srccitea>
<srccontr>Extent and altitude of bedrock units in the Nebraska part of the Sioux City 1-degree by 2-degree quadrangle.</srccontr>
</srcinfo>
<srcinfo>
<srccite>
<citeinfo>
<origin>COHYST</origin>
<pubdate>2006</pubdate>
<title>Testholes and wells used to delineate the base-of-aquifer altitude, COHYST study area</title>
<geoform>tabular digital data</geoform>
<serinfo>
<sername>Well and test-hole database used by COHYST</sername>
<issue>Issue identification, not specified</issue>
</serinfo>
<pubinfo>
<pubplace>Lincoln, Ne</pubplace>
<publish>Nebr. Dept. of Natural Resources</publish>
</pubinfo>
<othercit>Cooperative Hydrology Study data accessed on November 2006</othercit>
<onlink>http://cohyst.dnr.ne.gov/cohyst_preliminarydata.html</onlink>
</citeinfo>
</srccite>
<srcscale>250000</srcscale>
<typesrc>online</typesrc>
<srctime>
<timeinfo>
<sngdate>
<caldate>unknown</caldate>
</sngdate>
</timeinfo>
<srccurr>publication date</srccurr>
</srctime>
<srccitea>Testholes and wells, COHYST (2006)</srccitea>
<srccontr>Wells and testholes used to map the altitude of bedrock and configuration of the base of aquifer in the Cooperative Hydrology Study (COHYST) area.</srccontr>
</srcinfo>
<srcinfo>
<srccite>
<citeinfo>
<origin>Diffendal, Jr., R.F</origin>
<pubdate>1991</pubdate>
<title>Geologic maps showing configurations of bedrock surfaces, North Platte 1-degree by 2-degree quadrangle, Nebraska</title>
<geoform>raster digital data</geoform>
<serinfo>
<sername>U.S. Geological Survey Miscellaneous Investigations Series</sername>
<issue>Map I-2277</issue>
</serinfo>
<pubinfo>
<pubplace>Reston, Va</pubplace>
<publish>U.S. Geological Survey</publish>
</pubinfo>
<onlink>http://ngmdb.usgs.gov/Prodesc/proddesc_10209.htm</onlink>
</citeinfo>
</srccite>
<srcscale>250000</srcscale>
<typesrc>online and paper</typesrc>
<srctime>
<timeinfo>
<sngdate>
<caldate>unknown</caldate>
</sngdate>
</timeinfo>
<srccurr>publication date</srccurr>
</srctime>
<srccitea>Map I-2277</srccitea>
<srccontr>Extent and altitude of bedrock units in the North Platte 1-degree by 2-degree quadrangle.</srccontr>
</srcinfo>
<srcinfo>
<srccite>
<citeinfo>
<origin>Dreeszen, V.H.</origin>
<origin>Reed, E.C.</origin>
<origin>Burchett, R.R.</origin>
<origin>Prichard, G.E.</origin>
<pubdate>1973</pubdate>
<title>Bedrock geologic map showing thickness of overlying Quaternary deposits, Grand Island quadrangle, Nebraska and Kansas</title>
<geoform>raster digital data</geoform>
<serinfo>
<sername>U.S. Geological Survey Miscellaneous Investigations Series</sername>
<issue>Map I-819</issue>
</serinfo>
<pubinfo>
<pubplace>Reston, Va</pubplace>
<publish>U.S. Geological Survey</publish>
</pubinfo>
<onlink>http://ngmdb.usgs.gov/Prodesc/proddesc_9648.htm</onlink>
</citeinfo>
</srccite>
<srcscale>250000</srcscale>
<typesrc>online and paper</typesrc>
<srctime>
<timeinfo>
<sngdate>
<caldate>unknown</caldate>
</sngdate>
</timeinfo>
<srccurr>publication date</srccurr>
</srctime>
<srccitea>Map I-819</srccitea>
<srccontr>Extent of bedrock units in the Grand Island 1-degree by 2-degree quadrangle.</srccontr>
</srcinfo>
<srcinfo>
<srccite>
<citeinfo>
<origin>Eversoll, D.A.</origin>
<origin>Dreeszen, V.H.</origin>
<origin>Burchett, R.R.</origin>
<origin>Prichard, G.E.</origin>
<pubdate>1988</pubdate>
<title>Bedrock geologic map showing configuration of the bedrock surface, McCook 1-degree by 2-degree quadrangle, Nebraska and Kansas, and part of Sterling 1-degree x 2-degree quadrangle, Nebraska and Colorado</title>
<geoform>raster digital data</geoform>
<serinfo>
<sername>U.S. Geological Survey Miscellaneous Investigations Series</sername>
<issue>Map I-1878</issue>
</serinfo>
<pubinfo>
<pubplace>Reston, Va</pubplace>
<publish>U.S. Geological Survey</publish>
</pubinfo>
<onlink>http://ngmdb.usgs.gov/Prodesc/proddesc_9964.htm</onlink>
</citeinfo>
</srccite>
<srcscale>250000</srcscale>
<typesrc>online and paper</typesrc>
<srctime>
<timeinfo>
<sngdate>
<caldate>unknown</caldate>
</sngdate>
</timeinfo>
<srccurr>publication date</srccurr>
</srctime>
<srccitea>Map I-1878</srccitea>
<srccontr>Extent of bedrock units in the McCook 1-degree by 2-degree quadrangle.</srccontr>
</srcinfo>
<srcinfo>
<srccite>
<citeinfo>
<origin>Nebraska Department of Natural Resources</origin>
<pubdate>2007</pubdate>
<title>Registered wells database</title>
<geoform>vector digital data</geoform>
<pubinfo>
<pubplace>Lincoln, Ne</pubplace>
<publish>Nebraska Department of Natural Resources</publish>
</pubinfo>
<othercit>Nebraska Department of Natural Resources data accessed in July 2007</othercit>
<onlink>http://dnrdata.dnr.ne.gov/wellssql/</onlink>
</citeinfo>
</srccite>
<typesrc>online</typesrc>
<srctime>
<timeinfo>
<sngdate>
<caldate>unknown</caldate>
</sngdate>
</timeinfo>
<srccurr>publication date</srccurr>
</srctime>
<srccitea>Registered wells database, Nebraska</srccitea>
<srccontr>If a registered well was drilled to or below the base of the aquifer and the geologic log is sufficiently descriptive, the source provided the depth to the base of aquifer at the well location.</srccontr>
</srcinfo>
<srcinfo>
<srccite>
<citeinfo>
<origin>Nebraska Oil and Gas Commission</origin>
<pubdate>2007</pubdate>
<title>Oil and gas wells database</title>
<geoform>tabular digital data</geoform>
<serinfo>
<sername>Current database of oil and gas wells</sername>
<issue>Issue identification, not specified</issue>
</serinfo>
<pubinfo>
<pubplace>Sidney, Ne</pubplace>
<publish>Nebraska Oil and Gas Commission</publish>
</pubinfo>
<othercit>Nebraska Oil and Gas Commission data accessed May 2007</othercit>
<onlink>http://nogcc.ne.gov/</onlink>
</citeinfo>
</srccite>
<typesrc>online</typesrc>
<srctime>
<timeinfo>
<sngdate>
<caldate>unknown</caldate>
</sngdate>
</timeinfo>
<srccurr>publication date</srccurr>
</srctime>
<srccitea>Nebraska Oil and Gas Commission data</srccitea>
<srccontr>Altitude of bedrock units at well locations.</srccontr>
</srcinfo>
<srcinfo>
<srccite>
<citeinfo>
<origin>Pettijohn, R.A.</origin>
<origin>Chen, H.H.</origin>
<pubdate>1983</pubdate>
<title>Geohydrology of the High Plains Aquifer System in Nebraska</title>
<geoform>document</geoform>
<serinfo>
<sername>U.S. Geological Survey Open-File Report</sername>
<issue>82-502</issue>
</serinfo>
<pubinfo>
<pubplace>Reston, Va</pubplace>
<publish>U.S. Geological Survey</publish>
</pubinfo>
<onlink>http://pubs.er.usgs.gov/usgspubs/ofr/ofr82502</onlink>
</citeinfo>
</srccite>
<srcscale>750000</srcscale>
<typesrc>paper</typesrc>
<srctime>
<timeinfo>
<sngdate>
<caldate>unknown</caldate>
</sngdate>
</timeinfo>
<srccurr>publication date</srccurr>
</srctime>
<srccitea>OFR 82-502</srccitea>
<srccontr>This source includes a map of the base of the High Plains aquifer in Nebraska and of the geologic units that form the base of the aquifer. This source was visually compared to the current map of the base of aquifer and the extent of the geologic units that form the base of aquifer; the current maps were derived from this source and data acquired since this source was published.</srccontr>
</srcinfo>
<srcinfo>
<srccite>
<citeinfo>
<origin>Souders, V.L.</origin>
<pubdate>2000</pubdate>
<title>Geologic maps and cross sections showing configurations of bedrock surfaces, Broken Bow 1° x 2° quadrangle, east-central Nebraska</title>
<geoform>vector digital data</geoform>
<serinfo>
<sername>U.S. Geological Survey Miscellaneous Investigations Series</sername>
<issue>Map I-2725</issue>
</serinfo>
<pubinfo>
<pubplace>Reston, Va</pubplace>
<publish>U.S. Geological Survey</publish>
</pubinfo>
<onlink>http://ngmdb.usgs.gov/Prodesc/proddesc_28120.htm</onlink>
</citeinfo>
</srccite>
<srcscale>250000</srcscale>
<typesrc>online and paper</typesrc>
<srctime>
<timeinfo>
<sngdate>
<caldate>unknown</caldate>
</sngdate>
</timeinfo>
<srccurr>publication date</srccurr>
</srctime>
<srccitea>Map I-2725</srccitea>
<srccontr>Extent and altitude of bedrock units in the Broken Bow 1-degree by 2-degree quadrangle.</srccontr>
</srcinfo>
<srcinfo>
<srccite>
<citeinfo>
<origin>Swinehart, J.B.</origin>
<origin>Souders, V.L.</origin>
<origin>DeGraw, H.M.</origin>
<origin>Diffendal, Jr., R.F.</origin>
<pubdate>1985</pubdate>
<title>Cenozoic paleogeography of western Nebraska</title>
<geoform>document</geoform>
<lworkcit>
<citeinfo>
<origin>Flores, R.M.</origin>
<origin>Kaplan, S.S., eds.</origin>
<pubdate>1985</pubdate>
<title>Cenozoic paleogeography of west-central United States</title>
<geoform>document</geoform>
<pubinfo>
<pubplace>Denver, Co</pubplace>
<publish>Rocky Mountain Section, Society of Economic Paleontologist and Mineralogists</publish>
</pubinfo>
</citeinfo>
</lworkcit>
</citeinfo>
</srccite>
<srcscale>1250000</srcscale>
<typesrc>paper</typesrc>
<srctime>
<timeinfo>
<sngdate>
<caldate>unknown</caldate>
</sngdate>
</timeinfo>
<srccurr>publication date</srccurr>
</srctime>
<srccitea>Cenozoic paleogeography of western Nebraska</srccitea>
<srccontr>This source contains a configuration map of the base of the Ogallala Group and of the presence of the Ogallala Group in western Nebraska. This source was used to estimate drainage patterns in the current base-of-aquifer map and to identify areas where the Ogallala Group was not present.</srccontr>
</srcinfo>
<srcinfo>
<srccite>
<citeinfo>
<origin>Swinehart, J.B.</origin>
<origin>Diffendal, Jr., R.F.</origin>
<pubdate>1998</pubdate>
<title>Geology of the pre-dune strata</title>
<geoform>document</geoform>
<serinfo>
<sername>Resource Atlas</sername>
<issue>No. 5b, p. 29-42</issue>
</serinfo>
<lworkcit>
<citeinfo>
<origin>Bleed, A.S.</origin>
<origin>Flowerday, C.A., eds.</origin>
<pubdate>1998</pubdate>
<title>An atlas of the Sand Hills</title>
<geoform>document</geoform>
<serinfo>
<sername>Resource Atlas</sername>
<issue>No. 5b</issue>
</serinfo>
<pubinfo>
<pubplace>Lincoln, Ne</pubplace>
<publish>University of Nebraska-Lincoln, Conservation and Survey Division</publish>
</pubinfo>
</citeinfo>
</lworkcit>
</citeinfo>
</srccite>
<srcscale>1000000</srcscale>
<typesrc>paper</typesrc>
<srctime>
<timeinfo>
<sngdate>
<caldate>unknown</caldate>
</sngdate>
</timeinfo>
<srccurr>publication date</srccurr>
</srctime>
<srccitea>Geology of the pre-dune strata</srccitea>
<srccontr>This source contains a configuration map of the base of the Ogallala Group and of the presence of the Ogallala Group in the Sand Hills area in Nebraska. This source was used to estimate drainage patterns in the current base-of-aquifer contour map and to identify areas where the Ogallala Group was not present.</srccontr>
</srcinfo>
<srcinfo>
<srccite>
<citeinfo>
<origin>University of Nebraska-Lincoln, Conservation and Survey Division</origin>
<pubdate>2007</pubdate>
<title>Nebraska test-hole database</title>
<geoform>tabular digital data</geoform>
<pubinfo>
<pubplace>Lincoln, Ne</pubplace>
<publish>University of Nebraska-Lincoln, Conservation and Survey Division</publish>
</pubinfo>
<othercit>University of Nebraska-Lincoln, Conservation and Survey Division data accessed June 2007.</othercit>
<onlink>http://csd.unl.edu/general/testholes.asp</onlink>
</citeinfo>
</srccite>
<typesrc>online</typesrc>
<srctime>
<timeinfo>
<sngdate>
<caldate>unknown</caldate>
</sngdate>
</timeinfo>
<srccurr>publication date</srccurr>
</srctime>
<srccitea>Nebraska test-hole database</srccitea>
<srccontr>Altitude of bedrock units at test-hole locations.</srccontr>
</srcinfo>
<srcinfo>
<srccite>
<citeinfo>
<origin>U.S. Geological Survey and Nebraska Department of Natural Resources</origin>
<pubdate>1998</pubdate>
<title>7.5-minute digital elevation model--index for the State of Nebraska</title>
<serinfo>
<sername>Series name, not specified</sername>
<issue>Issue identification, not specified</issue>
</serinfo>
<pubinfo>
<pubplace>Lincoln, Ne</pubplace>
<publish>U.S. Geological Survey and Nebraska Department of Natural Resources</publish>
</pubinfo>
<othercit>Data accessed June 2006</othercit>
<onlink>http://dnr.ne.gov/databank/dem.html</onlink>
</citeinfo>
</srccite>
<srcscale>24000</srcscale>
<typesrc>online</typesrc>
<srctime>
<timeinfo>
<sngdate>
<caldate>unknown</caldate>
</sngdate>
</timeinfo>
<srccurr>publication date</srccurr>
</srctime>
<srccitea>DEM 10-m</srccitea>
<srccontr>This source was used to estimate the land surface altitude at each well and test-hole location.</srccontr>
</srcinfo>
<procstep>
<procdesc>The published and unpublished stratigraphic data were assembled from test-holes and wells records maintained by the Cooperative Hydrology Study (COHYST); Nebraska Department of Natural Resources; Nebraska Oil and Gas Commission; and the University of Nebraska-Lincoln, Conservation and Survey Division.</procdesc>
<srcused>COHYST base of aquifer data</srcused>
<srcused>Nebraska Oil and Gas Commission data</srcused>
<srcused>Nebraska test-hole database</srcused>
<srcused>Registered wells database, Nebraska</srcused>
<procdate>2007</procdate>
</procstep>
<procstep>
<procdesc>The geologic units that form the base of aquifer were plotted for each of the test-hole and registered wells and polygons were drawn on-screen for the areas with the same geologic unit forming the base of aquifer. The source data for test-holes and selected registered wells were re-examined when the designation for the  geologic unit that forms the base of aquifer was anomalous.  When needed, corrected values for the identity of the geologic unit that forms the base of aquifer were assigned, if known.

The land-surface altitude, as estimated by the 10-m DEM, was compared to the base-of-aquifer surface. Areas where the represented base-of-aquifer surface was above the estimated land surface was interpreted to be areas where either the base of aquifer surface was inaccurate or areas where the principal aquifer is thin or not present.</procdesc>
<procdate>2007</procdate>
</procstep>
<procstep>
<procdesc>The base-of-aquifer contours and the designation of the geologic unit that form the base of the aquifer were reviewed by geologists familiar with the area--E.D. Gutentag, U.S. Geological Survey (retired); J.B. Swinehart, University of Nebraska-Lincoln, Conservation and Survey Division; J.C. Cannia, U.S. Geological Survey; R.F. Diffendal, Jr., University of Nebraska-Lincoln, Conservation and Survey Division; and S.O. Lackey, University of Nebraska-Lincoln, Conservation and Survey Division. Their suggestions were incorporated into the dataset and the map.</procdesc>
<procdate>2007</procdate>
</procstep>
<procstep>
<procdesc>Metadata imported.</procdesc>
<srcused>P:\C8T02\GIS\aqbase\20090604_4approval_sim3042_gu.xml</srcused>
<procdate>20090604</procdate>
<proctime>12480400</proctime>
</procstep>
</lineage>
</dataqual>
<spdoinfo>
<direct>Vector</direct>
<ptvctinf>
<sdtsterm>
<sdtstype>Complete chain</sdtstype>
<ptvctcnt>166</ptvctcnt>
</sdtsterm>
<sdtsterm>
<sdtstype>Label point</sdtstype>
<ptvctcnt>40</ptvctcnt>
</sdtsterm>
<sdtsterm>
<sdtstype>GT-polygon composed of chains</sdtstype>
<ptvctcnt>41</ptvctcnt>
</sdtsterm>
</ptvctinf>
</spdoinfo>
<spref>
<horizsys>
<planar>
<gridsys>
<gridsysn>State Plane Coordinate System 1983</gridsysn>
<spcs>
<spcszone>2600</spcszone>
<lambertc>
<stdparll>40.000000</stdparll>
<stdparll>43.000000</stdparll>
<longcm>-100.000000</longcm>
<latprjo>39.833333</latprjo>
<feast>1640416.666667</feast>
<fnorth>0.000000</fnorth>
</lambertc>
</spcs>
</gridsys>
<planci>
<plance>coordinate pair</plance>
<coordrep>
<absres>15280</absres>
<ordres>15280</ordres>
</coordrep>
<plandu>Feet</plandu>
</planci>
</planar>
<geodetic>
<horizdn>North American Datum of 1983</horizdn>
<ellips>Geodetic Reference System 80</ellips>
<semiaxis>6378137.000000</semiaxis>
<denflat>298.257222</denflat>
</geodetic>
</horizsys>
</spref>
<eainfo>
<detailed>
<enttyp>
<enttypl>
sim3042_gu.pat</enttypl>
<enttypd>Feature attribute table for mapped polygons representing the geologic units that form the base of aquifer and areas where the base of aquifer is well defined.</enttypd>
<enttypds>See references listed in source information.</enttypds>
</enttyp>
<attr>
<attrlabl>FID</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>AREA</attrlabl>
<attrdef>Area of feature in internal units squared.</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Positive real numbers that are automatically generated.</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>PERIMETER</attrlabl>
<attrdef>Perimeter of feature in internal units.</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Positive real numbers that are automatically generated.</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>SIM3042_GU#</attrlabl>
<attrdef>Internal feature number.</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Sequential unique whole numbers that are automatically generated.</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>SIM3042_GU-ID</attrlabl>
<attrdef>User-defined feature number.</attrdef>
<attrdefs>ESRI</attrdefs>
<attrdomv>
<udom>Sequential unique whole numbers that were automatically generated.</udom>
</attrdomv>
</attr>
<attr>
<attrlabl>GEO_UNIT</attrlabl>
<attrdef>Identity of geologic units that form the base of the aquifer, or alternatively, a code signifying an area where the base of the principal aquifer is not well defined. Within the study area, the geologic units of the Lower Tertiary system generally are the Brule and Chadron Formation of the White River Group, but, for some test holes, the aquifer base was noted more generally as the White River Group. The geologic units of the Upper Cretaceous system are the Pierre Shale, Niobrara Formation, or Carlile Shale.</attrdef>
<attrdefs>See references listed in source information.</attrdefs>
<attrdomv>
<edom>
<edomv>LT</edomv>
<edomvd>A geologic unit of Lower-Tertiary age forms the base of aquifer in this area. These geologic units, in this area, generally are the Brule and Chadron Formation of the White River Group.</edomvd>
<edomvds>See references listed in source information.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>UK</edomv>
<edomvd>A geologic unit of Upper-Cretaceous age forms the base of aquifer in this area. These geologic units, in this area, generally are the Pierre Shale, Niobrara Formation of the Colorado Group, or the Carlie Shale of the Colorado Group.</edomvd>
<edomvds>See references listed in source information.</edomvds>
</edom>
</attrdomv>
<attrdomv>
<edom>
<edomv>NA</edomv>
<edomvd>The base of the principal aquifer is not well defined in this area.</edomvd>
<edomvds>See references listed in source information.</edomvds>
</edom>
</attrdomv>
</attr>
</detailed>
<overview>
<eaover>The relevant attributes for this dataset are: 
geo-unit, for the geologic units that form the base of aquifer and the areas where the aquifer is not well-defined.</eaover>
<eadetcit>See references listed in source information.</eadetcit>
</overview>
</eainfo>
<distinfo>
<distrib>
<cntinfo>
<cntorgp>
<cntorg>U.S. Geological Survey</cntorg>
</cntorgp>
<cntpos>Ask USGS - Water Webserver Team</cntpos>
<cntaddr>
<addrtype>mailing address</addrtype>
<address>507 National Center</address>
<city>Reston</city>
<state>Va</state>
<postal>20192</postal>
<country>USA</country>
</cntaddr>
<cntvoice>1-888-275-8747 (1-888-ASK-USGS)</cntvoice>
<cntemail>http://water.usgs.gov/user_feedback_form.html</cntemail>
<cntinst>Contact via email</cntinst>
</cntinfo>
</distrib>
<resdesc>Downloadable Data</resdesc>
<distliab>Although these data have been used by the U.S. Geological Survey, U.S. Department of the Interior, no warranty expressed or implied is made by the U.S. Geological Survey as to the accuracy of the data.  The act of distribution shall not constitute any such warranty, and no responsibility is assumed by the U.S. Geological Survey in the use of these data, software, or related materials.
	
The use of firm, trade, or brand names in this report is for identification purposes only and does not constitute endorsement by the U.S. Geological Survey.  The names mentioned in this document may be trademarks or registered trademarks of their respective trademark owners.</distliab>
<stdorder>
<digform>
<digtinfo>
<formname>ARCE</formname>
<formcont>Spatial and attribute information</formcont>
<filedec>Winzip</filedec>
<transize>0.5 Mbytes</transize>
</digtinfo>
<digtopt>
<onlinopt>
<computer>
<networka>
<networkr>http://water.usgs.gov/GIS/dsdl/sim3042gu_e00.zip</networkr>
</networka>
</computer>
</onlinopt>
</digtopt>
</digform>
<digform>
<digtinfo>
<formname>Shape</formname>
<formcont>Shape file</formcont>
<filedec>zipped</filedec>
<transize>1.0 Mbytes</transize>
</digtinfo>
<digtopt>
<onlinopt>
<computer>
<networka>
<networkr>http://water.usgs.gov/GIS/dsdl/sim3042gu_shp.zip</networkr>
</networka>
</computer>
</onlinopt>
</digtopt>
</digform>
<fees>None.  This dataset is provided by USGS as a public service.</fees>
</stdorder>
</distinfo>
<metainfo>
<metd>20090603</metd>
<metc>
<cntinfo>
<cntorgp>
<cntorg>U.S. Geological Survey</cntorg>
</cntorgp>
<cntpos>Ask USGS - Water Webserver Team</cntpos>
<cntaddr>
<addrtype>mailing</addrtype>
<address>455 National Center</address>
<city>Reston</city>
<state>VA</state>
<postal>20192</postal>
</cntaddr>
<cntvoice>1-888-275-8747 (1-888-ASK-USGS)</cntvoice>
<cntemail>http://answers.usgs.gov/cgi-bin/gsanswers?pemail=h2oteam&amp;subject=GIS+Dataset+sim3042gu</cntemail>
</cntinfo>
</metc>
<metstdn>FGDC Content Standards for Digital Geospatial Metadata</metstdn>
<metstdv>FGDC-STD-001-1998</metstdv>
<metsi>
<metscs>None</metscs>
<metsc>Unclassified</metsc>
<metshd>Not applicable</metshd>
</metsi>
</metainfo>
</metadata>
