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Table 7-1. Description of Geologic Units end Their Hydrologic Properties, <br />Seneca II-W Area <br />(Adapted Irom Brogden and Giles, 1977) <br /> Maximum <br /> Thldcness <br />System Series Geologic Unh Symbol (feet) ~ Physical Characteristip Hydroogic Charaderistia <br /> Dark-gray to bluish, homogenous, marine Reported well yields are less than 5 gal/ <br /> shale whh several thin Interbedded Mn. Water la predominantly a caldum <br /> aandstanes and calcareous conaetlons. bk:erbonate type. Dissolved-slide <br /> Lewis ooncentratlon ranges from 272 ro 4,230 <br /> Shale Kls 1,900 mgA. ~ Water may contain concentretlons <br /> of Iron, manganese, nhrate, selenium, and <br /> sullafe In excess o1 U.S. Public Health <br /> Servce (! 962) atandarda for drinking <br /> Upper water. <br /> Cretaceous Sardarone, NgM•brown to greylah•whlte, Reported well yields ere es much as 100 <br /> with Interbedded gray carbonaceous shale, geVrtYn, but average less then 10 gaVmin. <br /> mar, and linker beds. The wai beds rAwalg w@Ila Wfl YM IVIIIId PI IIUiI atlaa~l, <br /> Williams are al economic Impotence and more valleys and In areas where sandstones are <br /> Fork Kw 2,100 numerous than those of the Iles Fomatlon. overlain by Lewle Shale. Water Is <br /> Formation The very Ma to 9ne~relned, IlpMyray predominemly caldum end sodum <br /> ro white, massive, crossbedded Twentymlle bicarbonate types. Water In confect with <br /> 0 <br />Sandatona Merrbw Is • prominent ledge- <br />Ovate may be a caidurn satiate Type ar~d <br />n <br />'o ~ <br />Y <br />taming sandstone about 800 to 9001eB[ <br />canlaln 9uorlde, Iran, manganese, <br />u v above the bane 01 the lormation. selenium, and whale In exoeaa of U.S. <br />c A Interbedded IIgM-brown to whhe, massive, Publb Heahh Service (1962) standards fo <br />u ~ one-grolnad, ledge•foming sendarone, drlnldng water. Dissolved-colitis corx:en- <br /> brown rodads trarboneceous shale, sandy hatlan ranges Irom 334 to 1,460 rtgA end <br /> Iles shale, and Oval. The Trout Creek Sand averages 746 rtgA. Hydraulb-wnductiviry <br /> Formation KI 1,500 stone Member, a 50- to 100•It thldc, IIgM• values fa treclured aendstonea rerge Irom <br /> brown to IlgMyrey, fine-grained, messlvA 3.7 to 26 frld. <br /> sandstone, la located et the top of the <br /> lormatlon. <br /> Ughtgray to dark~rey fosslliferoua marine Reported well yields ere leas then 5 gaVmin. <br /> shale whh Interbedded sandstones end Ilme- Water Is predominemly a caldum bicar- <br /> sronea. The sandstones ere generally thM bonete type. Dissolved-solies concentration <br /> Upper bedded, Tina grained, tan, and lossllilerous, ranges fmm 338 to 2,590 rtgA. Water may <br /> and Mancoa and form resistant ledges In the basal end contain mncentratbns o1 chloride, huoride, <br /> Lower Shale Km 5,300 upper parts of the formation. The Overall Iron, end manganese In excess of U.S. <br /> Cretaceous arse oocupled by the Mancos Shale Is Public Heahh Service (1962) standards for <br /> characterized by a rolling hummocky drinking water. <br /> topography. <br />• • <br />