Buy Geological Survey Water-Supply Paper Volume 1587-1590 by Geological Survey
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Geological Survey Water-Supply Paper Volume 1587-1590

Geological Survey Water-Supply Paper Volume 1587-1590


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This historic book may have numerous typos and missing text. Purchasers can usually download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. Excerpt: ...older rocks are in fault contact. The anticline is terminated on both flanks by faults. The presence of another anticline in the southwestern part of the county is suggested by the relationship of the outcrops of the Midway and Navarro groups northeast of Macdona. This structure, whose axis strikes east-northeastward, is terminated at its southwest end by a cross fault. GROUND WATER IN THE EDWARDS AND ASSOCIATED LIMESTONES The principal water-bearing formation in Bexar County is the Edwards limestone. The underlying Comanche Peak limestone and the overlying Georgetown limestone also may be water bearing. Because well drillers do not distinguish them from the Edwards limestone, the three formations are considered in this report to constitute a single ground-water reservoir (aquifer) here called the Edwards and associated limestones. This aquifer is a continuous hydrologic unit along the Balcones fault zone from Kinney County on the west at least to Hays County on the northeast (Petitt and George, 1956). Where the Edwards and associated limestones crop out in the northern part of Bexar County (pll. 1), the water in them is confined only at the bottom by the relatively impermeable Glen Rose limestone; consequently, in this part of the county the water is under water-table conditions, and the water levels in wells are below the top of the aquifer. In the central and southern parts of the county, where the Edwards and associated limestones are buried beneath younger formations, the water is confined at the bottom by the Glen Rose limestone and at the top by the Grayson shale. Here the water is said to be under artesian conditions; that is, the water levels in wells are above the top of the aquifer, and in topographically low areas the wells may flow....


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Product Details
  • ISBN-13: 9781234041304
  • Publisher: Rarebooksclub.com
  • Publisher Imprint: Rarebooksclub.com
  • Height: 246 mm
  • No of Pages: 98
  • Spine Width: 5 mm
  • Width: 189 mm
  • ISBN-10: 1234041308
  • Publisher Date: 13 Jan 2013
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Weight: 191 gr


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