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Table III-C-2 cont ' d
<br /> in uro�dGad slit: ;ne, %hilt, and ll�.- �++tlgn aaallabls. sot tanatdarad
<br /> Chlnle
<br /> I,Ooo stcoa-p+abio cc,,glorrarota. AaddIsh an ayulfar In study area.
<br /> • ~ Triassic for:ution br�jhaly
<br /> lor.
<br /> i
<br /> s SfrolYe, with in"
<br /> silty Osta for Cnly one wall cbtalned; avatar f
<br /> lcmr anddturr-gralned sandstonas a calciva bicariacnace typo• ClSsolrsd-
<br /> Sl+ta
<br /> Triassic and yrldge 2,700 end silty s`.at.%. Aaddlsh brown anC soil,& ccncantratlta la �.5 a�g/i,
<br /> upper formatlon ,sIcarecus in places. Crossbadding
<br /> Parslan :d ripple marks locally present.
<br /> Varf'fine to svdlv,a-graiced, poorly sort- ko infor,-anon otollabla, NY 14 an =v'•l'
<br /> ed, red to gray sandstona with Inter- for In outcrop area.
<br /> F7, Upper ,abet l00 Lvdded siitston• and s:++le. TM grew
<br /> P&talon Sandstone color In tM tower bads is Cca to a
<br /> hydrocarbon stain on Quartz gralns.
<br /> W Sc_•+.e congloaaratas locally pravant.
<br /> Aed, calcareous, arkosic sandstone and Aaportud well fields rang• fraa 5 to 25
<br /> ,ne,a -taM Intern dUad slltstone, gal/aloe en.re fr aCtareJ er ronsfa ly,
<br /> tYa grayish-purple Itaas[gns, and arkosic say yield graatsr wantltlot of m: tr to
<br /> Loaf n9 co1WersL4. ConglCaenotaa are gad- wails. l--,;grunt so-fCd of water :n
<br /> ,acon lni
<br /> stall, passive, ccntang igneous, Carbondale area and Crystal tl wr
<br /> Jwlan ma ::rain•
<br /> and Upper 5,0�2 c•ta rphle, and Isolated llamstrne age Dasin. Voter la a cslclae bicarLcn•
<br /> Format iron
<br /> Iennsyl- bales. Sa:.dstgn•s and sM lap are eta type In iM Cattle Cfesk and Grbgn-
<br /> vanlan often mlG Kequf. nodular, and ,rtan sal♦ areas and a SoCiu+ bl4a.f4 .Sts typo
<br /> in the Crystal elver drainage basin. i
<br /> In color, Crasstadding and ripple y
<br /> marks are locally present. to 0lssoives .116 wcu n:;SL;Gtt ra.•y:.
<br /> lrCm 194 to 150 r9/1.
<br /> lnterbaddad gYpsun, der►-gray to black .'49ortad welt yields range from 5 90 25
<br /> shale, and gfpalfarcus siltstone. gal/min. USad as a roourca of water in
<br /> Shales are preae-ilnantly calcareous :d trA Carbondale and Cottle Croak prams.
<br /> s contain latarbeds of brew+lsh saadst -.a. rater is a calCiva suifat+ tYpe. 0ts-
<br /> _ N ;d1e Eagle CYpsure is generally suSsive, white, a�-_ solvad-solids eoneantrvticn ranges frc,a
<br /> a )a:nsYi- Ve1101 rev 3, weathara to a dark gray. TM formal Cr. 247 to 21630 +�9/1• TM octurrance of
<br /> y&nlM (vaporate as a whole waatrars to a yellowish-gray oateniva is localized; concantratlonS
<br /> rotor. sans Le45 ray be halltie. in excess of U.S. tir standards
<br /> ndaids Service
<br /> (l;bl) drinking-neater standard& occur
<br /> in the tattle Creek and Carbondale areas.
<br /> rtinturn Formation Llatstone, Balcalts, Sandstone, si)t• 3t0 Information available.
<br /> C,thic For"tion stone, antis, quartalte, and Sena
<br /> of LanganM la (1952) conglo�..rate. Aocks era generally
<br /> ttaidan Fcraation brownlah, light gray to dark gray,
<br /> ae
<br /> Lc-,or loadrtlle Llaasta• PC. 4,650 hard, calcareous, and >ay be sllghtly
<br /> • = o Par.na yl• to strongly i tanorpho rode
<br /> iMifae fors.aclon
<br /> wool+^ Hanl:oa 0olo-I to
<br /> end older
<br /> _ m Pear Leas forwatlon
<br /> L".aa Sa.aCCh (7uaf[elte
<br /> 19
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