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System <br />Quaternary Valley Fill Deposits <br />Cretaceous Dakota Sandstone <br />Jurassic Morrison Formation <br />Triassic <br />Curtis and Summerville <br />Formations <br />Permian and <br />Pennsylvanian <br />Entrada Sandsone <br />Glen Canyon and <br />Wingate Sandstone, <br />older Triassic rocks <br />Undevided <br />Mississippian Leadville Limestone <br />Devonian Undevided <br />Ordorvician <br />Cambrian <br />Precambrian Undevided <br />Geologic Unit Thick., Ft. <br />TABLE 2.04.5 -1 <br />SUMMARY OF GEOLOGIC UNITS AND HYDROLOGIC CHARACTERISTICS <br />Physical <br />20 -140 Clay, sand, gravel debris grading front coarse <br />Materials at head waters to finer materials down <br />stream. <br />< 300 Fine to coarse grained sandstones interbedded with <br />light gray to dark brown carbonaceous shales / siltstones <br />and coal. <br />250 -600 Varicolored siltstones and mudstone with beds of <br />sandstone and limestone <br />50 -200 Cross bedded sandstone, limestone, varicolored siltstone <br />with beds of sandstone and limestone <br />50 -200 Fine grained sandstone mostly crossbedded <br /><500 Sandstone, lenses of limestone, and varicolored <br />siltstone and mudstone. <br /><13,000 Shale, limestone, dolomite, congolmerate, and sandstone <br />50 -200 Limestone, dolomite. sandstone and chert <br /><2,500 Dolomite, limestone, quartzite, sandstone, congolmerate, <br />shale, and chert. <br />Granite, schist, gneiss, and pegmatite dikes. <br />Characteristics <br />Hydrological <br />Capable of yeilding 5 -100 gpm. Most having a hydrologic connection <br />with the stream. Water is commonly hard with varying amounts of <br />Ca, Mg, HCO and SO It is generally more mineralized than adjacent <br />stream. <br />Yields up to 400 gpm but for the most part much less. The water is <br />commonly saline, with Ca- Mg -SO or Na HCO Source for stock and <br />domestic wells. <br />Source of water for stock and domestic wells. <br />Source of water for stock and domestic wells. <br />Source of water for stock and domestic wells, locally yielding > 25 gpm. <br />Source of water for stock and domestic wells. <br />Sandstones yield saline water, not generally considered source for wells <br />Yields water from fractures and solution cavities, yields of >2.000 are <br />known, but extent of high yielding potential not known. <br />Small yields of potable water at depths < 2,000 feet <br />Yields water from fractures and weathered material, source of water for <br />both domestic and stock wells, generally yielding < 1 0gpm. <br />