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15 <br />CD <br />V <br />V <br />N <br />W <br />a .....x,....Ie <br />Y. <br />• <br />d.,..I.r <br />EXPLANATION OF HYDROLOGIC GROUPS <br />Nikes. Sandstone upper Unit sandstone and con. <br />Y <br />gimeerate: middle unit sandstone, carbonaceous <br />shelf/. and impure coal: lower it sandstone <br />and conglomerate. Gray. yello. and buff <br />coastal plain deposits. <br />y <br />m <br />❑ <br />Noenkopl Formation: upper volt Is predbminantTy <br />thin ripple - bedded shale middle unit Is pre- <br />dominantly arkosic sandstone and conglosan ta; <br />' lower unit is predominantly indistinctly bedded <br />2 mudstone, Gypsum occurs throughout the formation <br />e as thin seems and veins and bedded gypsum occurs <br />near the formation's base. Brown shallow marine <br />and fluvial deposits. <br />1 <br />Pervious sandstone and <br />carbonate bads <br />Impervious claystone, <br />- <br />Ring cengeds <br />h sparse b ads o/ <br />limestone end chert, liMite, gray, red, green <br />end purple fluvial ond lake deposits. <br />Cutler Formation; Arkosic sandstone and <br />conglomerate with Interbeds of sandy mudstone, <br />Sandy and silty IlmestOne Is present at the base <br />of the formation. Maroon, red and purple Inter- <br />Q calated continental and marine deposits. <br />O <br />sll[st one and eaapor Rte <br />pads <br />Limestone Member: Thick- bedded fosslliferous <br />limestone with beds of shale and minor arkose, <br />Gray marine deposits, <br />g 8 <br />E <br />paradox Member: Interbedded gypsum, anhydrite <br />halite limestone, shale and sandstone. Very <br />deformed due to plastic flowage. White, gray <br />and dark gray evaporites and shallow marine <br />deposits. <br />AUDENELS <br />:II Cete, (19 GI <br />111 Joesli . a d o.erl 1953 <br />older Paleozoic Rock., Sandstone, limestone <br />and dolomite. Marine deposits, <br />JD - 5 LEASE <br />Bedrock Slretlgraphy <br />chefs and associates, ma, <br />CONSULTIN ENGINEERS <br />a, OOP.] <br />+ r " ' <br />Prscaabrlan Rocks: Granite with Isolated dress <br />or quartzite. gneiss end schist. <br />Jell Nwmaw eu r•eo <br />0.. <br />18,101 Jf /N. 1110 Y's 2-8 <br />15 <br />CD <br />V <br />V <br />N <br />W <br />