Laserfiche WebLink
• Water quality generally degrades. becomes more saline, with depth as shown <br />schematically in FII'Lire S-S In addition, the amount of water generally decreases with <br />depth, with very little or no flow in some of the oil shale zones A generally accepted <br />interface between the presence of Ilovotio water and the lack of flowing water is known <br />as the Dissolution Surface Water has dissolved most of the soluhle salts above the <br />Dissolution Surface while soluble salts remain below the Dissolution Surface The <br />nahcolitic oil shale zone has -enerally not been exposed to flowin`, water and contains <br />soluble salts which are mined nearby us11111 solution minim, techniques in Class III UIC <br />wells The poor water quality near and below the Dissolution Surface generally <br />precludes that water from heing, classified as I ISDW <br />Recharged water moves through the <br />upper and lower bedrock aquifers <br />WEST and discharges to the stream volleys EA <br />-Recharge Recharge <br />• "".? fire E Valley-Fill <br />O0f P_ <br />r",Crpedd Upper par alluvium Upper aquifers <br />n k,?-er F k hlembdr t <br />arrria t'on <br />?aho9anY Zone of Parachute Cr rot Green River Formation <br />eek Membe Lower aquifers <br />dower Aart o/ Parachute <br />Creek "feibber <br />Garden Gulch Member of <br />Green River Formation and olde• racks <br />V?,,1dNA try m Taelnt tr . <br />Figure -1. Jchefnulic cJicwrcfm o/ Ille flrnr .vi•.ste in Ili the Pic 'educe ( 'Ivek ca'c'u, fi-oin <br />l iyywr uncl olller". , 2003. <br />• <br />8