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1988-04-11_PERMIT FILE - C1981008A (9)
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1988-04-11_PERMIT FILE - C1981008A (9)
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Last modified
1/5/2021 12:25:25 PM
Creation date
4/18/2012 2:35:43 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981008A
IBM Index Class Name
PERMIT FILE
Doc Date
4/11/1988
Doc Name
Hydrologic Description (Part 1 of 2)
Section_Exhibit Name
Tab 7
Media Type
D
Archive
Yes
Tags
DRMS Re-OCR
Description:
Signifies Re-OCR Process Performed
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Table ?-1. Summary of the Geologic Units and Hydrologic Character <br /> System Geologic Unit Thickness Physical Character Hydrological Character <br /> puaternary Valley Filled 20-140 Clay, sand, gravel debris, generally Capable of yielding 5 to 100 gFah, lost having a <br /> Deposits grading from coarse materials at hydrological o=v=ticn with the stream. Water <br /> the head waters to finer materials commonly is hard with varying amounts of Ca, <br /> darn stream. Mg, HOCY , and SO4. It is also generally more <br /> mineralized than adjacent stream . <br /> cretaceous Dakota Sandstone Up to 3000 Light to dark colored sandstone with Yields up to 400 gpm but for the most part much <br /> (including Biro interbeds of shale and coal. lose. The water is commonly saline. The water � <br /> Canyon Formation) comuonnly Ca-14g-SO4 or Na H003. <br /> -2 Jurassic Morrison Formation 250-600 Varicolored siltst o ne and mudstone Source of water to stock and dcmestin Nalls <br /> v with beds of sandstone and locally. <br /> limestone. <br /> Curtis and Summer- 50-200 Crossbedded sandstone, limestone. Source of water for stock and domestic walls. <br /> villa Formations varicolored siltstone and <br /> mndstone. <br /> Entrada Sandstone 50-200 Pine-grained sandstone. mostly Source of water for stock and domestic wuelI <br /> crossbedded. Locally yields more than 25 gpm. <br /> Triassic Glen Canyon and As thick Sandstone, lenses of limestone, and Sandstones are sources of water to stock and <br /> Wingate Sandstones as 500 varicolored siltstone and mid- domestic wells. <br /> and older Triassic stone. <br /> !locks <br /> Permian and Permian and Pennsyl- As thick Shale, limestone, dolomite, con- Sandstone beds cc manly yield saline water. <br /> �. Pennsylvanian vanian rocks as 13,000 glomerate, and sandstone. Not generally considered a source of water <br /> to well <br /> CDs. <br /> n <br /> o Mississippian Leadville Limestone 50-200 Limestone, dolomite, sandstone, Yields water from fractures and solution <br /> and chart. openings. Yields as much as several thousand <br /> gpm locally. Elkta nt of large yield potential <br /> �w is unknown. <br /> 00 <br /> Devonian Pre-Mississippian As thick Dolomite, limestone, quartzite, Yields small supplies of <br /> Ordovician rocks as 2,500 sandstone, conglomerate, shale, potable water at depths <br /> oong less than 2,000 feet. <br /> Cambrian and chert. <br /> Precambrian Precambrian rocks Granite, schist, gneiss, and Wells derive water from fractures and weathered <br /> pegmatite dikes. material. Source of water for damestic and <br /> stock supplies; yields are generally less than <br /> 10 cmn. <br />
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