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Table III-C-`_' cont ' d
<br /> --^-_ lnle ^intarcadCad 11it: +., thsla, and Sla+a- 1 'to inl_•-.atI, avaiic)Is. !'got con;lJtred
<br /> u i Up,er {h LOCO st.na-paabis cc �lcrarate. Radollh j An :,infer In study area.
<br /> Triassic For 40on brown +n color.
<br /> L
<br /> i Shaiy slltsIone, rlth ntarbeddad t!!ty 1 Oata Tcr rniy one Mall cbtalnoG, reset !s
<br /> Lc.+er State and shaly «dies-gralnad sandstoras i a CAICivn blcarto: le tys'-a• Olssdl+nd-
<br /> 1(lasalc and 9rld90 2,700 and silty At+lee. 0.cddlan bro.n and aollCa t.r.canirailrn Is
<br /> Uypor foratStac -+Icarecus in places. Crou bedd1nq
<br /> t TArelan d rl;pls marks locally present. —_
<br /> vsr I'fine to eadl:rr+-gralned, pr_orly sort- ' ko Infer*atlan a,oilaLle. NY Z 4 an •.;al•
<br /> ad, red to gray sandstone with Inter- for In outcrop area.
<br /> L.Ppar yabey lOG S+_Ca9 slitstona a•:d sh+le. Ttv gray
<br /> Tsrsslan Sandstone color Ia the f yr bads )s C..o to a
<br /> 1 hydrocarbon slain on quartz grain%.
<br /> t 6 I S,v cenglo"racas locally present. _
<br /> Calcarw wS. arkdsic sandstone and AeDcrtad ell yields range float5 to 25
<br /> 1 cn•++ Irk In[arceddea tsltt[one, ^vat/sin, +re fract-,.-I
<br /> � ..tenet. ly,
<br /> m gray l ah-parpto I,-a atone, and arua'c � y u Jlafd S star 4,4niltles of
<br /> L o,we cca q!we rate. CCaglcoeratss are Son- +,ells. Saywrtant 1"rca of .rater .t
<br /> T.ra.an Yrrcon *rally aussire, contalr,Ing Igneous. Carbonjale sraa and Crystal lllr.r. ..•aln-
<br /> an.d '.;•r+r roraatIots 5' +cet+•ac•rD!sle, and lulated Iic.astcno a2s :asln• vital is a celcits altar:.•+- +
<br /> pt—syl- pebbles. Sa 7stanas and shales are ate typ• In the Cattle Creak and Cst�-tt- i
<br /> vanlan often altar area, ^odrlar, and grain Gale areas and a sdG t+f+ i�ur*..=r tta ty;a
<br /> t In Color. Crosstsdding and rlpDle ;n tCe Crystal A1wr fralt4sSa reel,, i
<br /> ( ' larks are locally present. of saoi.w-ao:f.s w`nc•n::silo, r«•ir..
<br /> 11 fn_s 194 to t,15D :.9/1.
<br /> I Intarbsdded gyps +, =.rk-Srsy to Slack •a�ortad .a11 ylald% rarSs floe S to YS
<br /> 1,a14, ant St;.alfsro•as 111tstone. gal;eln. Used as a t"CCS of +.star In
<br /> S*slss Ara yredc..{ra^tiy :alearsort tro Carbondale and Cattle Creak sraas.
<br /> scoctsin latarbeda of Drc+.nish a n's; 'Hater is a calci w sulfata tyD+,
<br /> dte Cagis 4yDs•aa Is weraily nasslre, mite, C solvad-sollds concantratIw rwjs3 frog
<br /> Tc ,Ayl. Valley ?ev 3, .natners to a dark gray. Tna foraat;c 247 to 2,630 ng/1. Tlse occurrence of
<br /> vanlen [vaporise as a vt+ola .sAtt•'s to • y*Ila.ish-gray sslanlve is tocailaad; ccrcantretlons
<br /> wlor. Sucre be.s ty be halltle.
<br /> In •.Cass of U.S. tt,bllc >lealth Service
<br /> drinktng-meter standards utur
<br /> in the Cattle Creak and Carbondale areas.
<br /> r ,turn ror"tlon lL+sstana, Lolcaalts, sandstone, silt- ;:o inroraatlon ava11aS1e.
<br /> _.thic ror:atlon st.na, anala, yuartaito. .nd so•4 1
<br /> of Langanhai• (15521 conglc.erate. Aocks are generally I
<br /> 9aldan rcratlon brownish, Ilght gray to dark gray,
<br /> Lowrey Loads111e CI:aMeta• PC. 1,b50 11410, CAICAr-0-l. and .ay be si l•gttly
<br /> N a� Ter.syl• {half,• rur.atlon to atrongly •�a tan+o r;�o led.
<br /> v unlan K•nl•�u Oil uel 4.e
<br /> end olGer � Pearl .11 forA.O.
<br /> ac" '� .a.•ccn 4uartalte
<br /> 19
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