Laserfiche WebLink
i•'v~1 is - 1_. .. ~ ~ _ .•. , _ .. <br />- jjti--Ccbb17:, Cla~:ey ?ands, Steen <br />- - This a complex of shal.los% tc r.,cdcracly dcc}~, c:et.l drair:<•d soils <br />.. -an zccteratnl7 c,tcen to stre,r ric!;;•; are} }_a,,,_lilce :~rca:: in the f::othill <br />' --~~'~-ea..._-.That' arc forisin~ in cobbly end ~s•a:'clly calcarc:~ur cln;~ey allu•:iai <br />- rnt_rials o•rerlyir.; shale.. The ne^ra;;c annual prccipit~~.t.tnn i:; about <br />:l~~to'1y irc!les, ;rust free season is l~`i to 11~O.days an9 neon nn•.ma1 <br />- -' -t.C^OerattL^C 1S abn'lt l;On F. ae~;~tia.^. ra^~;es ` `^ ''" <br />_ from, ~O:,v to u~~~; ..."cot. <br />::~ . - - . . <br />..._ .The maderatel;: cicep cobbt.:Y and rra~•c}ly clay -loam soils [sa::c un. - <br />a~oat 40 ocrc_~nt o: the unit ocr.u}ryin the mid slope posiCicn :ith ~~ <br />- .'slopes of 15 to j0 percent.=~ These soils arc urdcrla:n by male at _ , <br />depths of ~0 to 4^ inches. The s~allc:r cobbly- claf loc- soils ~:ave un_ <br />- .. aoout 2C percen+. and ere on crest sloe=_ a*d knob-1x}:~ a.cas :;here t:-~e <br />citale for..^..ati on is less than ;'r? inches beneath the surface. <br />,• <br />,. ; . <br />s: <br />.:~. <br />r"' ; <br />;:,:.. <br /> <br />".Inc'_ucied in this unit are amall areas of Denver ~{t~'tsclly clay loa- <br />~.'' . <br />_ on sloncs o^ y to 15 percent in the scope: position:. P,lso, inclusior:,' <br />! ;: of ^arroa rid_re too areas of cobbly t}cderlard soils on slopes of 1 to ' <br />_ 5 percent; , <br />i ; <br />• - <br />`~:':•~.;,; P^_Tme3hlllt~l5 slo:;, a•railable water ca_~acity ran~,es fror low an <br />.--~:::~;: t:'°:snallow soils .on ridge crests to high on the m:~deretcly dec!•~ cl.aye;,~ <br />t: <br />' ~`%v ~i` s~ils.t'~'-i'si`fe ctive:. raotin~ depth •rarics SrC,:~~1~,1GCI:9 •:"t 0.~!l'? 1nC!I~_.^.. _ <br />t.T.:- .- <br />~' _- Surface runoff is hz~h, crater croc_on hnr.ard:is hich. These ..:i.ls are.'. <br />..;m_erate alkalina and dii'ficult to till 'oecause of the cLayfsur.ace . <br />":"~~=-arsi,subsoil layers. Shriek-swell potential is.hi.;h. <br />w. <br />s %~~?;:_i ~ This complex is u-ed mairi?f for livestock grazing, sildlife Ord `~ <br />- - .:'ecreatian. Some. areas are used fcr building. s~tE°.devei:pr,:ent. r ' <br />F .. <br />_'~,;x= =`'Corunw;ity Dcvelonment - Th1s cb-}rle:c has sednre timitntior_; I'or -~ ~ _ <br />'=~"'= ~"'~'ii~ld't^~ site a:~d~rer_re_ational dei'clo~rent:; - a].ope, shrinl_ssrell s~i~l., <br />" :::,end death '.a shale,. Soil aroA.^, Ilced for ;,hose i,urpore require special <br />~''`~~-;v'eSioR:;"POat1h~S should be desiCred to: prevent, structural dan:a[;e caused <br />.-, ~- <br />"`:-.bj s*irinkina and: swelling of they sail and bedrock. ~'; <br />`_'`~ - - - <br />,"';5'•-N ... , .'.' c .. i;•t:; gC`C'Dll.^.h On <br />``" Flant.lldantation - Pants 4r.d Iaorn., are difficul. __ , <br />~~ £ivsersoila, Srecial care ancLmcasures arr r~qu:re•1 to cr_per...ctc <br />Y. r . <br />.-„no. _ ia„a't,= rate, coob7.v ur_'acc lagers or, i;cos ar.:) c _•~=_ i` ti_i, ;;;;::. _ <br />_-':,;i=and slc~e. Eackfilliog :rit.h sandy and :carry topscil, incc-•r~ratin .'. <br />:y.-`.plant residue^ into surface layer and grading slo;_s are ef~ecti~e • <br />```reesu~es aid'n~ establis!~~eat of plant and grass CoVCr. <br />,~. <br />'"~Ad~.a.~>.t~f: w.. ~.:.+,•:R:R J! ':sT4>,Y`<~: jri. '7 :wJ". ,;r:-°'d'~;_- "r~'..7.^~.SN!Zl:': ^.`~`.~'""y=Ff <br />.., r='v~ ..-.~'i+ .S°~~. T ~~tTi'Yt~"'i~:f~~~ -~PF.i~:' .. <br />, <br />