1996
DOI: 10.3133/ha730e
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Ground Water Atlas of the United States: Segment 4, Oklahoma, Texas

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Cited by 8 publications
(12 citation statements)
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“…The Edwards-Trinity aquifer system is composed of three aquifers of Cretaceous-age carbonate and clastic rocks, which are described in detail by Ryder (1996) and George and others (2011) and summarized here: from west to east, the aquifers are the Edwards-Trinity aquifer, the Edwards aquifer, and the Trinity aquifer. The Edwards aquifer overlies and is in part hydraulically connected to the Trinity aquifer, whereas the Trinity and Edwards-Trinity aquifers are stratigraphically equivalent in part and are hydraulically connected in places (Ryder, 1996). The climate of the region is highly variable with mean annual precipitation decreasing from east to west by an order of magnitude.…”
Section: Edwards-trinity Aquifer System Principal Aquifer Study Netwomentioning
confidence: 99%
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“…The Edwards-Trinity aquifer system is composed of three aquifers of Cretaceous-age carbonate and clastic rocks, which are described in detail by Ryder (1996) and George and others (2011) and summarized here: from west to east, the aquifers are the Edwards-Trinity aquifer, the Edwards aquifer, and the Trinity aquifer. The Edwards aquifer overlies and is in part hydraulically connected to the Trinity aquifer, whereas the Trinity and Edwards-Trinity aquifers are stratigraphically equivalent in part and are hydraulically connected in places (Ryder, 1996). The climate of the region is highly variable with mean annual precipitation decreasing from east to west by an order of magnitude.…”
Section: Edwards-trinity Aquifer System Principal Aquifer Study Netwomentioning
confidence: 99%
“…The stream-valley aquifers are associated with the sand and gravel deposits in the valleys of the stream or river that typically is hydraulically connected to the aquifers (Miller and Appel, 1997); consequently, these aquifers usually are only as much as a few miles wide but can extend over long distances (Ryder, 1996). These aquifers typically are no more than 100 ft thick, but along some of the large rivers may be as much as 160 ft thick (Miller and Appel, 1997).…”
Section: Stream-valley Aquifers Principal Aquifer Study Network 1 (Stmentioning
confidence: 99%
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“…The study area is in the Great Plains physiographic province (fig. 1) and consists of an elevated and relatively undissected plain (Ryder, 1996). The study area covers about 3,225 mi 2 , including 1,525 mi 2 in LEUWCD, 798 mi 2 in SLUWCD, and 902 mi 2 in SPUWCD (fig.…”
Section: Description Of Study Areamentioning
confidence: 99%
“…The combination of minimal topographic relief, availability of groundwater for irrigation, and excellent soils makes this an important agricultural region in Texas (Ryder, 1996). From the USGS National Land Cover Database (NLCD) 2011, the land-cover categories for rangeland (shrubs/scrubs [31 percent] and grassland/herbaceous [19 percent]) and for cultivated crops (42 percent) dominate in the study area (fig.…”
Section: Description Of Study Areamentioning
confidence: 99%