<?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>Runkle, Donna</origin>
				<origin>Rea, Alan</origin>
				<origin>Source data sets and supplemental information
provided by Scott Christenson
				</origin>
				<pubdate>1997</pubdate>
				<title>Digital data sets that describe aquifer characteristics of the Central Oklahoma aquifer in central Oklahoma</title>
				<edition>1.0</edition>
				<geoform>map</geoform>
				<serinfo>
					<sername>Open-File Report</sername>
					<issue>96-454</issue>
				</serinfo>
				<pubinfo>
				<pubplace>Reston, VA</pubplace>
				<publish>U.S. Geological Survey</publish>
				</pubinfo>
				<onlink>http://water.usgs.gov/lookup/getspatial?ofr96-454_wlelev</onlink>
			</citeinfo>
		</citation>
		<descript>
			<abstract>This data set consists of digitized water-level elevation
contours for the Central Oklahoma aquifer in central
Oklahoma. This area encompasses all or part of Cleveland,
Lincoln, Logan, Oklahoma, Payne, and Pottawatomie
Counties. The Central Oklahoma aquifer includes the alluvial
and terrace deposits along major streams, the Garber
Sandstone and Wellington Formations, and the Chase, Council
Grove, and Admire Groups. The Quaternary-age alluvial and
terrace deposits consist of unconsolidated clay, silt, sand,
and gravel. The Permian-age Garber Sandstone and Wellington
Formations consist of sandstone with interbedded siltstone
and mudstone. The Permian-age Chase, Council Grove, and
Admire Groups consist of sandstone, shale, and thin
limestone.

The Central Oklahoma aquifer underlies about 3,000 square
miles of central Oklahoma where the aquifer is used
extensively for municipal, industrial, commercial, and
domestic water supplies. Most of the usable ground water
within the aquifer is from the Garber Sandstone and Wellington
Formations. Substantial quantities of usable ground water
also are present in the Chase, Council Grove, and Admire
Groups, and in alluvial and terrace deposits associated with
the major streams.

The water-level elevation map was created from digital data
sets developed to produce a map for a previously published
report. Water-levels measured in wells during the winter of
1986 and 1987 were used to construct the map. The digital
data set contains water-level elevations that range from 850
to 1,350 feet above sea level or the National Geodetic
Vertical Datum of 1929 (NGVD29).
			</abstract>
			<purpose>This data set was created for a project to develop data sets to
support ground-water vulnerability analysis. The objective was
to create and document a digital geospatial data set from a
published report or map, or existing digital geospatial data
set that could be used in ground-water vulnerability analysis.
			</purpose>
			<supplinf>Introduction --

This data set consists of digitize water-level elevation
contours for the Central Oklahoma aquifer in central
Oklahoma. This area encompasses all or part of Cleveland,
Lincoln, Logan, Oklahoma, Payne, and Pottawatomie Counties. The
Central Oklahoma aquifer includes the alluvial and terrace
deposits along major streams, the Garber Sandstone and
Wellington Formations, and the Chase, Council Grove, and Admire
Groups described in the report, "Ground-water-quality assessment
of the Central Oklahoma aquifer, Oklahoma: Geochemical and
Geohydrologic Investigations," by Parkhurst, Christenson, and
Breit (1996). The Quaternary-age alluvial and terrace deposits
consist of unconsolidated clay, silt, sand, and gravel. The
Permian-age Garber Sandstone and Wellington Formations consist
of sandstone with interbedded siltstone and mudstone. The
Permian-age Chase, Council Grove, and Admire Groups consist of
sandstone, shale, and thin limestone (Parkhurst, Christenson,
and Breit, 1996).

The Central Oklahoma aquifer underlies about 3,000 square
miles of central Oklahoma where the aquifer is used
extensively for municipal, industrial, commercial, and
domestic water supplies. Most of the usable ground water
within the aquifer is from the Garber Sandstone and Wellington
Formations. Substantial quantities of usable ground water
also are present in the Chase, Council Grove, and Admire
Groups, and in alluvial and terrace deposits associated with
the major streams (Parkhurst, Christenson, and Breit, 1996).

The water-level elevation map was prepared and published at a
scale of 1:250,000 as figure 2 on sheet 1 of the report,
"Hydrogeologic maps of the Central Oklahoma aquifer,
Oklahoma," by Christenson, Morton, and Mesander (1992) from
water-levels measured in wells during the winter of 1986 and
1987. The digital water-level elevation data set in this
report was created from the digital data sets developed to
produce the maps in Christenson, Morton, and Mesander (1992).

In this report, elevation refers to distance above sea level
and sea level refers to the National Geodetic Vertical Datum
of 1929 (NGVD29)--a geodetic datum derived from a general
adjustment of the first-order level nets of both the United
States and Canada, formerly called Sea Level Datum of
1929. The digital data set contains water-level elevations
that range from 850 to 1,350 feet above sea level or NGVD29.

Reviews Applied to Data --

This electronic report was subjected to the same review standard
that applies to all U.S. Geological Survey reports. Reviewers
were asked to check the topological consistency, tolerances,
attribute frequencies and statistics, projection, and geographic
extent. Reviewers were given digital data sets and paper plots
for checking against the source maps to verify the linework and
attributes. The reviewers checked the metadata and a_readme.1st
files for completeness and accuracy.

Related Spatial and Tabular Data Sets --

This data set is one of four digital map data sets being published
together for this aquifer. The four data sets are:

&gt;              aqbound -  aquifer boundaries

&gt;              cond    -  hydraulic conductivity

&gt;              recharg -  aquifer recharge

&gt;              wlelev  -  water-level elevation contours

Digital map data sets of the Oklahoma surficial geology digitized from
1:250,000-scale maps (or 1:125,000-scale maps for the three Oklahoma
panhandle counties) are published separately.

Other References Cited --

Christenson, S.C., Morton, R.B., and Mesander, B.A., 1992,
Hydrogeologic maps of the Central Oklahoma aquifer, Oklahoma:
U.S. Geological Survey Hydrologic Investigations Atlas HA-724,
3 sheets, scale 1:250,000

Douglas, D.H., and Peucker, T.K., 1973, Algorithm for the
reduction of the number of points required to represent a
digitized line or its caricature, Canadian Cartographer, 10,
No. 2 (December 1973)

Environmental Systems Research Institute, Inc. (ESRI), 1995,
ARC/INFO Command Reference, ARC/INFO On-line manuals:
Redlands, CA.

Parkhurst, D.L., Christenson, Scott, Breit, G.N., 1996,
Ground-water-quality assessment of the Central Oklahoma
aquifer, Oklahoma: Geochemical and geohydrologic
investigations: U.S. Geological Water-Supply Paper 2357, 101 p.

Notes --

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 data set has 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 and related materials.

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 this data, software, or related materials.
			</supplinf>
		</descript>
		<timeperd>
			<timeinfo>
				<rngdates>
					<begdate>1986</begdate>
					<enddate>1987</enddate>
				</rngdates>
			</timeinfo>
			<current>ground condition</current>
		</timeperd>
		<status>
			<progress>Complete</progress>
			<update>None planned</update>
		</status>
		<spdom>
			<bounding>
				<westbc>-97.6624</westbc>
				<eastbc>-96.8013</eastbc>
				<northbc>35.9971</northbc>
				<southbc>34.9183</southbc>
			</bounding>
		</spdom>
		<keywords>
			<theme>
				<themekt>none</themekt>
				<themekey>ground-water vulnerability</themekey>
				<themekey>groundwater vulnerability</themekey>
				<themekey>aquifers</themekey>
				<themekey>ground water</themekey>
				<themekey>groundwater</themekey>
				<themekey>Central Oklahoma aquifer</themekey>
				<themekey>Garber Sandstone</themekey>
				<themekey>Wellington Formation</themekey>
				<themekey>Chase Group</themekey>
				<themekey>Council Grove Group</themekey>
				<themekey>Admire Group</themekey>
				<themekey>ground-water levels</themekey>
				<themekey>groundwater levels</themekey>
				<themekey>water levels</themekey>
				<themekey>ground-water level elevation</themekey>
				<themekey>groundwater level elevation</themekey>
				<themekey>ground-water level elevation contours</themekey>
				<themekey>groundwater level elevation contours</themekey>
				<themekey>water-level elevation contours</themekey>
				<themekey>water level elevation contours</themekey>
				<themekey>water-level contours</themekey>
				<themekey>water level contours</themekey>
				<themekey>water-level elevation</themekey>
				<themekey>water level elevation</themekey>
				<themekey>inlandWaters</themekey>
			</theme>
			<place>
				<placekt>none</placekt>
				<placekey>central Oklahoma</placekey>
			</place>
		</keywords>
		<accconst>None.</accconst>
		<useconst>This data set represents the water-level elevation contours
that were created for and published at a scale of 1:250,000
in the report by Christenson, Morton, and Mesander (1992)
from water-levels measured in wells during the winter of 1986
and 1987. Water-level elevation contours represented at this
scale are indicative of broad, regional trends and should not
be interpreted as site specific.
		</useconst>
		<ptcontac>
			<cntinfo>
				<cntperp>
					<cntper>Donna L. Runkle</cntper>
					<cntorg>U.S. Geological Survey</cntorg>
				</cntperp>
				<cntpos>Hydrologist</cntpos>
				<cntaddr>
					<addrtype>mailing address</addrtype>
					<address>202 NW 66th St., Bldg. 7</address>
					<city>Oklahoma City</city>
					<state>Oklahoma</state>
					<postal>73116</postal>
					<country>United States of America</country>
				</cntaddr>
				<cntvoice>1-888-275-8747</cntvoice>
				<cntfax>(405) 843-7712</cntfax>
				<cntemail>dlrunkle@usgs.gov</cntemail>
				<cntinst>none</cntinst>
			</cntinfo>
		</ptcontac>
		<browse>
			<browsen>http://water.usgs.gov/lookup/get?OFR96-454/browse.gif</browsen>
			<browsed>A browse image of the four aquifer data sets.</browsed>
			<browset>GIF</browset>
		</browse>
		<datacred>Compilation of this data set and the associated metadata was
funded under a cooperative Joint Funding Agreement between the
U.S. Geological Survey and the State of Oklahoma, Office of
the Secretary of Environment.
		</datacred>
		<secinfo>
			<secsys>Public</secsys>
			<secclass>UNCLASSIFIED</secclass>
			<sechandl>None</sechandl>
		</secinfo>
		<native>Operating System-- UNIX, ARC/INFO Version 7.0.3,(Mon Mar 13 22:21:55 PST 1995)
		</native>
	</idinfo>
	<dataqual>
		<logic>Chain-node topology present.</logic>
		<complete>This data set includes all the water-level elevation contours
published on figure 2, sheet 1, in a report by Christenson,
Morton, and Mesander (1992).
		</complete>
		<posacc>
			<horizpa>
				<horizpar>None</horizpar>
				<qhorizpa>
					<horizpav>64 meters</horizpav>
					<horizpae>Resolution as reported</horizpae>
				</qhorizpa>
			</horizpa>
			<vertacc>
				<vertaccr>None.</vertaccr>
			</vertacc>
		</posacc>
		<lineage>
			<procstep>
				<procdesc>The digital aquifer boundary data set in this report was
copied from the digital data sets developed to produce the
figures in Christenson, Morton, and Mesander (1992). Map
projection information was not stored with the original data
sets, therefore, the map projection information, Universal
Transverse Mercator (UTM) project, zone 14, North American
Datum of 1927 (NAD27) documented in Christenson, Morton, and
Mesander (1992) was added using the ARC/INFO PROJECTDEFINE
command (ESRI, 1995). The projection was later converted to
the Albers Conical Equal Area, North American Datum of 1983
(NAD83) using the ARC/INFO PROJECT command (ESRI, 1995).
				</procdesc>
				<procdate>19970425</procdate>
			</procstep>
			<procstep>
				<procdesc>The data set was edited and dangling nodes
were removed. The lines were attributed for ELEV and LTYPE.
				</procdesc>
				<procdate>19970515</procdate>
			</procstep>
			<procstep>
				<procdesc>The paper plot of the data set was compared
to the published maps in Christenson, Morton, and Mesander (1992)
to verify the location and labels of lines in the data set.
				</procdesc>
				<procdate>19970515</procdate>
			</procstep>
			<procstep>
				<procdesc>The data set was documented using ARC/INFO DOCUMENT.AML (ESRI, 1995).</procdesc>
				<procdate>19970515</procdate>
			</procstep>
			<procstep>
				<procdesc>The ARC/INFO GENERALIZE command (Douglas and Peucker, 1973)
with a weed tolerance of 64 meters to reduce the number of
vertices representing the water-level elevation contours. The
reduction of vertices decreased the size of the ARC/INFO data
set to 5 percent of its original size. The generalized coverage was
compared with the original coverage on the computer screen to
verify that the location and shape of the lines remained the
same. A paper plot of the data set also was compared to the
published maps in Christenson, Morton, and Mesander (1992) to
verify the location and shape of lines remained the same.
				</procdesc>
				<procdate>19970527</procdate>
			</procstep>
		</lineage>
	</dataqual>
	<spdoinfo>
		<direct>Vector</direct>
		<ptvctinf>
			<sdtsterm>
				<sdtstype>Point</sdtstype>
			</sdtsterm>
			<sdtsterm>
				<sdtstype>String</sdtstype>
				<ptvctcnt>110</ptvctcnt>
			</sdtsterm>
			<sdtsterm>
				<sdtstype>GT-polygon composed of chains</sdtstype>
			</sdtsterm>
		</ptvctinf>
	</spdoinfo>
	<spref>
		<horizsys>
			<planar>
				<mapproj>
					<mapprojn>Albers Conical Equal Area</mapprojn>
					<albers>
						<stdparll>29.5</stdparll>
						<stdparll>45.5</stdparll>
						<longcm>-96</longcm>
						<latprjo>23</latprjo>
						<feast>0.0</feast>
						<fnorth>0.0</fnorth>
					</albers>
				</mapproj>
				<planci>
					<plance>coordinate pair</plance>
					<coordrep>
						<absres>64 meters</absres>
						<ordres>64 meters</ordres>
					</coordrep>
					<plandu>METERS</plandu>
				</planci>
			</planar>
			<geodetic>
				<horizdn>North American Datum of 1983</horizdn>
				<ellips>Geodetic Reference System 80</ellips>
				<semiaxis>6378137</semiaxis>
				<denflat>298.257</denflat>
			</geodetic>
		</horizsys>
	</spref>
	<eainfo>
		<detailed>
			<enttyp>
				<enttypl>WLELEV.AAT</enttypl>
				<enttypd>Attribute table of WLELEV.</enttypd>
				<enttypds>ARC/INFO</enttypds>
			</enttyp>
			<attr>
				<attrlabl>-</attrlabl>
				<attrdef>Attribute table of WLELEV.</attrdef>
				<attrdefs>ARC/INFO</attrdefs>
				<attrdomv>
					<edom>
						<edomv>-</edomv>
						<edomvd>n/a</edomvd>
						<edomvds>n/a</edomvds>
					</edom>
				</attrdomv>
			</attr>
			<attr>
				<attrlabl>FNODE#</attrlabl>
				<attrdef>Internal number of from-node</attrdef>
				<attrdefs>Computed</attrdefs>
				<attrdomv>
					<edom>
						<edomv>Sequential unique positive integer</edomv>
						<edomvd>n/a</edomvd>
						<edomvds>n/a</edomvds>
					</edom>
				</attrdomv>
			</attr>
			<attr>
				<attrlabl>TNODE#</attrlabl>
				<attrdef>Internal number of to-node</attrdef>
				<attrdefs>Computed</attrdefs>
				<attrdomv>
					<edom>
						<edomv>Sequential unique positive integer</edomv>
						<edomvd>n/a</edomvd>
						<edomvds>n/a</edomvds>
					</edom>
				</attrdomv>
			</attr>
			<attr>
				<attrlabl>LPOLY#</attrlabl>
				<attrdef>Internal number of poly to left of arc</attrdef>
				<attrdefs>Computed</attrdefs>
				<attrdomv>
					<edom>
						<edomv>Sequential unique positive integer</edomv>
						<edomvd>n/a</edomvd>
						<edomvds>n/a</edomvds>
					</edom>
				</attrdomv>
			</attr>
			<attr>
				<attrlabl>RPOLY#</attrlabl>
				<attrdef>Internal number of poly to right of arc</attrdef>
				<attrdefs>Computed</attrdefs>
				<attrdomv>
					<edom>
						<edomv>Sequential unique positive integer</edomv>
						<edomvd>n/a</edomvd>
						<edomvds>n/a</edomvds>
					</edom>
				</attrdomv>
			</attr>
			<attr>
				<attrlabl>LENGTH</attrlabl>
				<attrdef>Length of arc in coverage units</attrdef>
				<attrdefs>Computed</attrdefs>
				<attrdomv>
					<edom>
						<edomv>Positive real numbers</edomv>
						<edomvd>n/a</edomvd>
						<edomvds>n/a</edomvds>
					</edom>
				</attrdomv>
			</attr>
			<attr>
				<attrlabl>WLELEV#</attrlabl>
				<attrdef>Internal feature number</attrdef>
				<attrdefs>Computed</attrdefs>
				<attrdomv>
					<edom>
						<edomv>Sequential unique positive integer</edomv>
						<edomvd>n/a</edomvd>
						<edomvds>n/a</edomvds>
					</edom>
				</attrdomv>
			</attr>
			<attr>
				<attrlabl>WLELEV-ID</attrlabl>
				<attrdef>User-assigned feature number</attrdef>
				<attrdefs>User-defined</attrdefs>
				<attrdomv>
					<edom>
						<edomv>Integer</edomv>
						<edomvd>n/a</edomvd>
						<edomvds>n/a</edomvds>
					</edom>
				</attrdomv>
			</attr>
			<attr>
				<attrlabl>ELEV</attrlabl>
				<attrdef>Water-level contour elevation in feet above NGVD29</attrdef>
				<attrdefs>Christenson, Morton, and Mesander (1992)</attrdefs>
				<attrdomv>
					<rdom>
						<rdommin>850</rdommin>
						<rdommax>1,350</rdommax>
					</rdom>
				</attrdomv>
			</attr>
			<attr>
				<attrlabl>LTYPE</attrlabl>
				<attrdef>Line type</attrdef>
				<attrdefs>Christenson, Morton, and Mesander (1992)</attrdefs>
				<attrdomv>
					<edom>
						<edomv>1</edomv>
						<edomvd>n/a</edomvd>
						<edomvds>n/a</edomvds>
					</edom>
				</attrdomv>
			</attr>
			<attr>
				<attrlabl>MAJOR1</attrlabl>
				<attrdef>Water-level contour elevation in feet above NGVD29</attrdef>
				<attrdefs>Christenson, Morton, and Mesander (1992)</attrdefs>
				<attrdomv>
					<rdom>
						<rdommin>850</rdommin>
						<rdommax>1,350</rdommax>
					</rdom>
				</attrdomv>
			</attr>
			<attr>
				<attrlabl>MINOR1</attrlabl>
				<attrdef>Line type</attrdef>
				<attrdefs>Christenson, Morton, and Mesander (1992)</attrdefs>
				<attrdomv>
					<edom>
						<edomv>1</edomv>
						<edomvd>n/a</edomvd>
						<edomvds>n/a</edomvds>
					</edom>
				</attrdomv>
			</attr>
		</detailed>
		<overview>
			<eaover>Two attributes are associated with each line in this digital
data set. The first attribute, ELEV, contains the elevation
of the water-level contour, expressed in feet above the
National Geodetic Vertical Datum of 1929 (NGVD29). The second
attribute, LTYPE, contains a code that indicates the line is
solid on the source map.  ELEV is stored in the first major
code (MAJOR1) and LTYPE is stored in the first minor code
(MINOR1) for lines in the Digital Line Graph (DLG) version of
this data set.
			</eaover>
			<eadetcit>See overview.</eadetcit>
		</overview>
	</eainfo>
	<distinfo>
		<distrib>
			<cntinfo>
				<cntorgp>
					<cntorg>U.S. Geological Survey</cntorg>
				</cntorgp>
				<cntpos>Ask USGS - Water Webserver Team</cntpos>
				<cntaddr>
					<addrtype>mailing</addrtype>
					<address>445 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+ofr96-454_wlelev</cntemail>
			</cntinfo>
		</distrib>
		<distliab>Although this data set has 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 and related materials. 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 this data, software, or 
related materials.

Any use of trade, product, or firm names is for descriptive
purposes only and does not imply endorsement by the U.S.
Government.</distliab>
		<stdorder>
			<digform>
				<digtinfo>
					<formname>Export</formname>
					<formcont>Full coverage</formcont>
					<filedec>zipped</filedec>
					<transize>1</transize>
				</digtinfo>
				<digtopt>
					<onlinopt>
						<computer>
							<networka>
								<networkr>http://water.usgs.gov/GIS/dsdl/ofr96-454_wlelev.e00.gz</networkr>
							</networka>
						</computer>
					</onlinopt>
				</digtopt>
			</digform>
			<digform>
				<digtinfo>
					<formname>Other</formname>
					<formcont>DLG file format</formcont>
					<filedec>zipped</filedec>
					<transize>1</transize>
				</digtinfo>
				<digtopt>
					<onlinopt>
						<computer>
							<networka>
								<networkr>http://water.usgs.gov/GIS/dsdl/ofr96-454_wlelev.dlg.gz</networkr>
							</networka>
						</computer>
					</onlinopt>
				</digtopt>
			</digform>
			<fees>None. This dataset is provided by USGS as a public service.</fees>
		</stdorder>
	</distinfo>
	<metainfo>
		<metd>20041108</metd>
		<metc>
			<cntinfo>
				<cntorgp>
					<cntorg>U.S. Geological Survey</cntorg>
				</cntorgp>
				<cntpos>Ask USGS -- Water Webserver Team</cntpos>
				<cntaddr>
					<addrtype>mailing</addrtype>
					<address>445 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+ofr96-454_wlelev</cntemail>
			</cntinfo>
		</metc>
		<metstdn>FGDC Content Standards for Digital Geospatial Metadata</metstdn>
		<metstdv>FGDC-STD-001-1998</metstdv>
	</metainfo>
</metadata>
