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Table IIT_-C-2
<br /> Foaar:pti_1 of ;10:c;:d �iita izmd t}air F.�+ry oJia pr;wrttaa
<br /> i r.rstam !.ties ,aotr-gle unit ;fsooi ;hlCxness ThtaIcaI c h a r a c t a r I s t I t!ydrolegic chArsctsrlstics
<br /> If*10 1
<br /> Clay, sl It, sar,J, 9r1re1, a,d ^cullers. Aa;,ortsd .a 11 yields are is •::ch as is
<br /> Colluvlum Qc so Caneratly poorly tartad and ar.guier. gaf/eln. Souris of s.at:r for rang
<br /> Formed as a res.lt of C,hrls mccuwu- i apr1rg4, valor ,—I lty d.;,_r:ant ,n
<br /> IstIon at foot of slopes. ;.r.uoIItIon of parent .-a:arlsi.
<br /> ar, silt, sand, and gravel. Ce,oslts 'uported ..all yleils ars s► �m.c: vt 75
<br /> .ra cvo4arstoly to poorly sorted and cal/min. 9—,,a,tent aorru of rats, In
<br /> ' ii ^slat of althor an;ulsr or ra.nded Cart-, .Isis arse. Vitar a.ai!ty .)r 1a':1.
<br /> fro;sn1a. a,d done 104nt Is �Gar lying .)drr.k •,J
<br /> I
<br /> riolacene %�.,rca of all—;at r.tarlal, Wstar !a a
<br /> 1 r.alclun wifsts type )r a Calcl•.e sr-
<br /> Altuvly. Qal 200 typo. ols solv.d-tol1es c.a, )-
<br /> tratian Qantas f"I 2A5 to 1,450 aviI
<br /> Sal:nip, oc Curs In -'Cass
<br /> r with Ssrvlca {1, ;I CrlrRing- Jtsr I
<br /> :tender ds •.hare al�.,vi u-a !s In
<br /> with tma E.9is Valley (vapor)u. ''r.r;a-
<br /> tic C..n .:tivlty vaf„as r.ngo fr.a 1.0 1
<br /> I{ f:/d !n the Cattle Creak valley is i:4
<br /> f ' ft/d !n tha Aoarinq form, Alver valley.
<br /> 011.;ns basalt, dark-gray, eweratalr to anportad ,.e!I yields -svaral!y rangs fr::a
<br /> 1 htghly vesicular and often dense. Cc-a- 2�a 3imin; fields cf I':0 p);/a!n
<br /> >-nly jointed and fractured and veath- are ,rot unc,-,acxrs In e;liapsad erase. t
<br /> ars to a raddlsl4brov.n color. ' 2xs4lt is primary source of ma tar la tal-
<br /> i t!s Creak draina;s basin; to infora,ati:�s
<br /> ^lalstxens It QD I,000 available for basalt in .astern rare of
<br /> Crystal River drainepe basin. :stir is
<br /> A
<br /> Calclua blcarbciats type. Dlasolvad-
<br /> solIds ewcantraticn ranges from I11 ,
<br /> 475 pg/i. Hydraulic conductivity sal s
<br /> 1 rang. from 1.0 to 40 ft/4.
<br /> TII:Cmse Pradoelnaatly granod;orlte aid quartz No Infoe-.ation available, kot an a, 1Far
<br /> Igneous rocks TI tndau r- morurniu, light-gray to brc..n, --dtxr In study area.
<br /> ► minate grained, lansa, anJ hard. Fracturing
<br /> ort
<br /> c ':1 i;xana
<br /> .c and Jointing coc+a .
<br /> � C1aYstons, ra.dstone, and spate with In- No infarzaticn available. hat vn ssalfar
<br /> :ual th tub.da of alltstcne and cenglrete. In sty area. 1
<br /> A'ocane fo r.at Ion J Tr 6,CC0 ux ud
<br /> .arsar grained beds tend to be arloslc 1
<br /> and lenticular.
<br /> Intorbaddad sandstone, shalt' card, shale, Data ,for only one ,ell c7,alned, +.star is
<br /> an4 teal. Sandstones are can In cover, • calci w bls.aroonata type. Di ssulva4-
<br /> ^saverde lLsv 2,700 Passive, and £e rw prminsnt ridges, solids tutcantratian Is 191 wg/i.
<br /> FC atlon Shelas are green iin gray and locally
<br /> Upper csrbonaceous. Coals are aconcnlcaliy i
<br /> Cratac)•aua I.Wrtant. 11
<br /> c Dark-gray seals. wltn Interbedded sand- Data for only one .nil cbtalnod; Maur Ia
<br /> •' _ !!Antos stone, aiItsteno, and tiroestana. a cslclun bicarbonsto typo. 0140 va4-
<br /> Shale %w 4,u00 Scales are calcareous and aI'ghtIy solids concantrazlcn is 237 sg/i.
<br /> - car✓onacaous. Locally fossiliferous.
<br /> u
<br /> P reda.1 nantly Iignt-gray, very fine to ' Nv 1 Info r_+atIon avaI Iabla. May :a, an ayul 6av u S )dstona avedlun, weII-sorted, we11-cenenled, for csltcrop area.
<br /> w Lnr and sandstone with she le and sIItstone
<br /> Cretaceous eurre C.nyon l 300 interbads.. Chart-patble, congturerates -
<br /> Formation are coarxm. The sandstone eathers to
<br /> a rust-bro..n color and forms ridges.
<br /> Varicolored shale with intaroadded light- No laformaticn avelleDls. 114y t�s to agal-
<br /> gray sandstone and slltstono and Cara- far In outcrop area.
<br /> tsorrltc+a gray Iiarestona. Saristono beds are
<br /> Fors4n on 325 tors prcninant In the tower part of
<br /> the formation; IIPes.tone bads, in the
<br /> gaper middle. i
<br /> � JurasalG >Ju
<br /> Sand%ono, Is I i.;wlsh-gray to gray, very No inforratlon sva;lsblo. flay be an c.;,ul•
<br /> Entrada ISO floe :a =sdiun, ,..I1-sertsd, cress- t Far in euterop area.
<br /> .dndstone ba&od, and calcarwus. "<at".e rt to
<br /> zn ;rdngt-gray co'.or; forts
<br /> Upper Chin„a 1 Intaresddad aIItit rot, spats, and Z'r�- :o IrN matIon )vsllable. "at C,.stdirid
<br /> ' Trla,a;G For^stoon i t.CCO t� stwo-psablo caiglc-e nia. A427ish .n aqulfar In steCy drys.
<br /> ! brc-i in color.
<br /> Lc.nr I Shaly slltstcns, with lntsrbaedad slit, Da a for only one .,ell ab�alasd; wetar fa
<br /> 'rlsssit xnd 'taco and shaiy avvdlsi-gralr.ed sandstoass a calcluw hlcsrtacnwts rypi. olsv)I
<br /> �,,yef 9rlGge 3,7Co and silty shales. ?addlsh bran and solids t -:4,1tratlon is ;..3 r->3/i.
<br /> 1 J forAa!!on catca•aous In pl.cas. Crossdeddlrg
<br /> P3-,lan 11
<br /> L— and ripple Marks :cc at ly ,;;cser,t. —
<br /> 1
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