<?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>Adams, Gregory P.</origin>
				<origin>Runkle, Donna</origin>
				<origin>Rea, Alan</origin>
				<pubdate>1997</pubdate>
				<title>Digital data sets that describe aquifer characteristics of the alluvial and terrace deposits along the Beaver-North Canadian River from the panhandle to Canton Lake in northwestern Oklahoma</title>
				<edition>1.0</edition>
				<geoform>map</geoform>
				<serinfo>
					<sername>Open-File Report</sername>
					<issue>96-446</issue>
				</serinfo>
				<pubinfo>
				<pubplace>Reston, VA</pubplace>
				<publish>U.S. Geological Survey</publish>
				</pubinfo>
				<onlink>http://water.usgs.gov/lookup/getspatial?ofr96-446_aqbound</onlink>
			</citeinfo>
		</citation>
		<descript>
			<abstract>This data set consists of digital aquifer boundaries for the
alluvial and terrace deposits along the Beaver-North Canadian
River from the panhandle to Canton Lake in northwestern
Oklahoma. Ground water in 830 square miles of the Quaternary-age
alluvial and terrace aquifer is an important source of water for
irrigation, industrial, municipal, stock, and domestic supplies.
The aquifer consists of poorly sorted, fine to coarse,
unconsolidated quartz sand with minor amounts of clay, silt, and
basal gravel. The hydraulically connected alluvial and terrace
deposits unconformably overlie the Tertiary-age Ogallala
Formation and Permian-age formations.

The aquifer boundaries established in a ground-water flow model
for the aquifer include areas: 1) where the terrace deposits
pinch out against relatively impermeable Permian-age formations;
2) where the alluvium has been deposited against relatively
impermeable Permian-age formations; 3) where the alluvial and
terrace deposits have been eroded and underlying Permian-age
formations are exposed at the surface; 4) where the aquifer
extends beyond the geographic limit of the study area; and 5)
where the aquifer has little or no saturated thickness.

The lines in the data set representing aquifer boundaries
along geological contacts were extracted from a published
digital surficial geology data set based on a scale of
1:250,000. The geographic limits of the aquifer and areas of
little or no saturated thickness were digitized from a folded
paper map, at a scale of 1:250,000 from a ground-water
modeling report.
			</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
sets that could be used in ground-water vulnerability analysis.
			</purpose>
			<supplinf>Introduction --

This data set consists of digital aquifer boundaries for the
alluvial and terrace deposits along the Beaver-North Canadian
River from the panhandle to Canton Lake in northwestern
Oklahoma. Ground water in 830 square miles of the Quaternary-age
alluvial and terrace aquifer is an important source of water for
irrigation, industrial, municipal, stock, and domestic supplies.
The aquifer consists of poorly sorted, fine to coarse,
unconsolidated quartz sand with minor amounts of clay, silt, and
basal gravel. The hydraulically connected alluvial and terrace
deposits unconformably overlie the Tertiary-age Ogallala
Formation and Permian-age formations (Davis and Christenson, 1981).

The aquifer boundaries established in a ground-water model
report (Davis and Christenson, 1981) about the aquifer include
areas: 1) where the terrace deposits pinch out against
relatively impermeable Permian-age formations; 2) where the
alluvium has been deposited against relatively impermeable
Permian-age formations; 3) where the alluvial and terrace
deposits have been eroded and underlying Permian-age formations
are exposed at the surface; 4) where the aquifer extends beyond
the geographic limit of the study area; and 5) where the aquifer
has little or no saturated thickness.

The lines in the data set representing aquifer boundaries along
geological contacts were extracted from a published digital
surficial geology data set (Cederstrand, 1996) based on a scale
of 1:250,000. The geographic limits of the aquifer and areas of
little or no saturated thickness were digitized from a folded
paper map, at a scale of 1:250,000 from the ground-water
modeling report, "Geohydrology and numerical simulation of the
alluvium and terrace aquifer along the Beaver-North Canadian
River from the panhandle to Canton Lake, northwestern Oklahoma,"
by Davis and Christenson (1981, plate 3).

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 --

Cederstrand, J.R., 1996, Digital geologic map of Woodward
quadrangle, northwest Oklahoma: U.S. Geological Survey
Open-File Report 96-381, based on a scale of 1:250,000, 2
diskettes. (Available in nonproprietary and ARC/INFO formats.)
URL:http://wwwok.cr.usgs.gov/gis/geology/index.html

Davis, R.E. and Christenson, S.C., 1981, Geohydrology and numerical
simulation of the alluvium and terrace aquifer along the
Beaver-North Canadian River from the Panhandle to Canton Lake,
northwestern Oklahoma: U.S. Geological Survey Open-file Report
81-483, 42 p., 15 pl.

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

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>
				<sngdate>
					<caldate>1981</caldate>
				</sngdate>
			</timeinfo>
			<current>publication date</current>
		</timeperd>
		<status>
			<progress>Complete</progress>
			<update>None planned</update>
		</status>
		<spdom>
			<bounding>
				<westbc>-99.9650</westbc>
				<eastbc>-98.5487</eastbc>
				<northbc>36.9727</northbc>
				<southbc>36.0439</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>North Canadian River alluvial and terrace aquifer</themekey>
				<themekey>North Canadian alluvial and terrace aquifer</themekey>
				<themekey>Beaver River alluvial and terrace aquifer</themekey>
				<themekey>Beaver alluvial and terrace aquifer</themekey>
				<themekey>alluvial and terrace aquifer</themekey>
				<themekey>terrace aquifer</themekey>
				<themekey>alluvial aquifer</themekey>
				<themekey>terrace</themekey>
				<themekey>terrace deposit</themekey>
				<themekey>alluvium</themekey>
				<themekey>aquifer boundary</themekey>
				<themekey>inlandWaters</themekey>
			</theme>
			<place>
				<placekt>none</placekt>
				<placekey>northwestern Oklahoma</placekey>
			</place>
		</keywords>
		<accconst>None.</accconst>
		<useconst>Features representing aquifer boundaries along geological
contacts were extracted from a digital geology data set by
Cederstrand (1996) based on a scale of 1:250,000. Boundaries
defining the geographic limits of the aquifer and areas of
little or no saturated thickness were digitized from a folded
paper map (30 inches by 22 inches), at a scale of 1:250,000
(Davis and Christenson, 1981, plate 3). The digitized aquifer
boundaries had a maximum registration root-mean-squared-error
(RMSE) of 0.017 map inches (0.043 map centimeters) or 354.0 feet
(107.90 meters) ground distance. Boundaries 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?OFR96-446/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>
		<crossref>
			<citeinfo>
				<origin>Cederstrand, Joel R.</origin>
				<pubdate>1996</pubdate>
				<title>Digitized geology of Woodward quadrangle,
northwestern Oklahoma
				</title>
				<edition>1.0</edition>
				<geoform>map</geoform>
				<serinfo>
					<sername>Open-File Report</sername>
					<issue>96-381</issue>
				</serinfo>
				<pubinfo>
					<pubplace>Oklahoma City, OK</pubplace>
					<publish>U.S. Geological Survey</publish>
				</pubinfo>
				<onlink>http://wwwok.cr.usgs.gov/gis/geology/index.html</onlink>
			</citeinfo>
		</crossref>
	</idinfo>
	<dataqual>
		<logic>Chain-node topology present.</logic>
		<complete>This data set includes the aquifer boundaries published on plate 3
by Davis and Christenson (1981). Aquifer boundaries with a value
of 2 for the LSOURCE line attribute were taken from Cederstrand
(1996).
		</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 features representing aquifer boundaries along geological
contacts were extracted from digital geology data sets using
the ARC/INFO GET command (ESRI, 1995). The ARC/INFO CLEAN
command (ESRI, 1995) was used to process the polygon data set
using a dangle length of 0.0 feet or meters and fuzzy
tolerance of 32.8 feet (10.0 meters). The ARC/INFO PROJECT
command (ESRI, 1995) was used to convert the extracted data
set projection from Albers Conical Equal Area to Universal
Transverse Mercator-Zone 14.
				</procdesc>
				<procdate>1996</procdate>
			</procstep>
			<procstep>
				<procdesc>The geographic limits of the aquifer and areas of little or no
saturation thickness were digitized from a folded paper
map, at a scale of 1:250,000.
				</procdesc>
				<procdate>1996</procdate>
			</procstep>
			<procstep>
				<procdesc>Ten registration tics, located at township and range corners,
were projected into Universal Transverse Mercator-Zone 14,
which was the projection used for manual digitizing. The
aquifer boundaries were digitized in two sessions with a maximum
registration root-mean-squared error (RMSE) of 0.017 inches
(0.043 centimeters) map distance or 354.0 feet (107.90 meters)
ground distance.
				</procdesc>
				<procdate>1996</procdate>
			</procstep>
			<procstep>
				<procdesc>The data set was edited to delete extraneous pseudo and dangle
nodes. The ARC/INFO CLEAN command (ESRI, 1995), was used with
a dangle length of 32.8 feet (10.0 meters) and fuzzy tolerance
of 0.0 feet or meters.
				</procdesc>
				<procdate>1996</procdate>
			</procstep>
			<procstep>
				<procdesc>The registration tics used in the initial digitizing were
township and range corners taken form 1:24,000-scale
topographic maps. A comparison of a paper plot of the data set
with the source map showed that the township and range corners
were not in the same locations on the 1:250,000-scale source
map. To correct the problem a 1:250,000-scale U.S. Geological
Survey quadrangle map was registered using latitudinal and
longitudinal registration tics, with a maximum
root-mean-squared-error (RMSE) of 0.003 inches (0.007
centimeters) map distance or 72.97 feet (22.24 meters) ground
distance. Ten registration tics were selected and digitized
from the quadrangle map, and given the same tic identification
numbers as the tics that were used initially. These new tics
were used with the ARC/INFO TRANSFORM command (ESRI, 1995) to
adjust the digitized lines to more closely match the source
map. The registration root-mean-squared-error (RMSE) for
TRANSFORM was 403.90 feet (123.11 meters) ground distance or
0.019 map inches (0.048 map centimeters).
				</procdesc>
				<procdate>1996</procdate>
			</procstep>
			<procstep>
				<procdesc>The ARC/INFO PROJECT command (ESRI, 1995) was used to convert
the data set projection from Universal Transverse
Mercator-Zone 14 to Albers Conical Equal Area.
				</procdesc>
				<procdate>1996</procdate>
			</procstep>
			<procstep>
				<procdesc>The ARC/INFO CLEAN command (ESRI, 1995) was used with a dangle
length of 32.8 feet (10.0 meters) and fuzzy tolerance of 0.0
feet or meters. Polygons were attributed for AQTYPE and
lines were attributed LSOURCE. Verification of attribute codes
were made by comparing a paper plot of the data set with the
source map.
				</procdesc>
				<procdate>1996</procdate>
			</procstep>
		</lineage>
	</dataqual>
	<spdoinfo>
		<direct>Vector</direct>
		<ptvctinf>
			<sdtsterm>
				<sdtstype>Point</sdtstype>
				<ptvctcnt>10</ptvctcnt>
			</sdtsterm>
			<sdtsterm>
				<sdtstype>String</sdtstype>
				<ptvctcnt>28</ptvctcnt>
			</sdtsterm>
			<sdtsterm>
				<sdtstype>GT-polygon composed of chains</sdtstype>
				<ptvctcnt>11</ptvctcnt>
			</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>AQBOUND.PAT</enttypl>
				<enttypd>Polygon attribute table of AQBOUND</enttypd>
				<enttypds>ARC/INFO</enttypds>
			</enttyp>
			<attr>
				<attrlabl>-</attrlabl>
				<attrdef>Polygon attribute table of AQBOUND</attrdef>
				<attrdefs>ARC/INFO</attrdefs>
				<attrdomv>
					<edom>
						<edomv>-</edomv>
						<edomvd>n/a</edomvd>
						<edomvds>n/a</edomvds>
					</edom>
				</attrdomv>
			</attr>
			<attr>
				<attrlabl>AREA</attrlabl>
				<attrdef>Area of polygon in square 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>PERIMETER</attrlabl>
				<attrdef>Perimeter of polygon 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>AQBOUND#</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>AQBOUND-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>AQTYPE</attrlabl>
				<attrdef>Aquifer type</attrdef>
				<attrdefs>Davis and Christenson (1981)</attrdefs>
				<attrdomv>
					<edom>
						<edomv>1,2,3</edomv>
						<edomvd>n/a</edomvd>
						<edomvds>n/a</edomvds>
					</edom>
				</attrdomv>
			</attr>
			<attr>
				<attrlabl>MAJOR1</attrlabl>
				<attrdef>Aquifer type</attrdef>
				<attrdefs>Davis and Christenson (1981)</attrdefs>
				<attrdomv>
					<edom>
						<edomv>1,2,3</edomv>
						<edomvd>n/a</edomvd>
						<edomvds>n/a</edomvds>
					</edom>
				</attrdomv>
			</attr>
			<attr>
				<attrlabl>MINOR1</attrlabl>
				<attrdef>Blank item for DLG</attrdef>
				<attrdefs>Calculated</attrdefs>
				<attrdomv>
					<edom>
						<edomv>0</edomv>
						<edomvd>n/a</edomvd>
						<edomvds>n/a</edomvds>
					</edom>
				</attrdomv>
			</attr>
		</detailed>
		<detailed>
			<enttyp>
				<enttypl>AQBOUND.AAT</enttypl>
				<enttypd>Arc attribute table</enttypd>
				<enttypds>ARC/INFO</enttypds>
			</enttyp>
			<attr>
				<attrlabl>-</attrlabl>
				<attrdef>Arc attribute table</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 polygon 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 polygon 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>AQBOUND#</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>AQBOUND-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>LSOURCE</attrlabl>
				<attrdef>Source of line</attrdef>
				<attrdefs>Davis and Christenson (1981),
Cederstrand (1996)
				</attrdefs>
				<attrdomv>
					<edom>
						<edomv>1,2</edomv>
						<edomvd>n/a</edomvd>
						<edomvds>n/a</edomvds>
					</edom>
				</attrdomv>
			</attr>
			<attr>
				<attrlabl>MAJOR1</attrlabl>
				<attrdef>Source of line</attrdef>
				<attrdefs>Davis and Christenson (1981),
Cederstrand (1996)
				</attrdefs>
				<attrdomv>
					<edom>
						<edomv>1,2</edomv>
						<edomvd>n/a</edomvd>
						<edomvds>n/a</edomvds>
					</edom>
				</attrdomv>
			</attr>
			<attr>
				<attrlabl>MINOR1</attrlabl>
				<attrdef>Blank item for DLG</attrdef>
				<attrdefs>Calculated</attrdefs>
				<attrdomv>
					<edom>
						<edomv>0</edomv>
						<edomvd>n/a</edomvd>
						<edomvds>n/a</edomvds>
					</edom>
				</attrdomv>
			</attr>
		</detailed>
		<overview>
			<eaover>Each polygon in this data set has an associated attribute,
AQTYPE, with values of 1 representing areas where the aquifer is
present, 2 representing areas where the aquifer is absent or
areas not considered part of the aquifer, and 3 representing
areas where the aquifer was too thin (little or no saturated
thickness) for modelng ground-water flow (Davis and Christenson,
1981). AQTYPE is stored in the first major code (MAJOR1) for
polygons, and 0 is stored in the first minor code (MINOR1) in
the Digital Line Graph (DLG) version of this data set.

Each line in this digital data set has an associated attribute,
LSOURCE, that contains a code to indicate the line source. An
LSOURCE code of 1 indicates the line was digitized from Davis
and Christenson (1981), and an LSOURCE code of 2 indicates the
line was extracted from Cederstrand (1996). LSOURCE is stored in
the first major code (MAJOR1) for lines, and 0 is stored in the
first minor code (MINOR1) 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+ofr96-446_aqbound</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/ofr96-446_aqbound.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/ofr96-446_aqbound.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+ofr96-446_aqbound</cntemail>
			</cntinfo>
		</metc>
		<metstdn>FGDC Content Standards for Digital Geospatial Metadata</metstdn>
		<metstdv>FGDC-STD-001-1998</metstdv>
	</metainfo>
</metadata>
