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r=0R3E5 ht.INE <br />~ECTIIJN II - SOILS IhJVEPiTORr <br />Oltrerent Iinds of soil, range sites, or woodland sites are separated on <br />the raep by solid b1acl~:: lln?s. Withln each ar?a is an rdenttfying syrrbel <br />OY name. The TO I lO~Ni ng 5y'iiiGO1S 31' Shov.,n On your iiiap: <br />,vmboi or .te (Jame G?neralized D?scriations <br />Soils Descriptions (Oe±afled d?scriations are .available <br />In yn~ir x.011 I_On SeY Vat lOn v?I-'J1~=? <br />!]Y11re. 1_ <br />FiF Louviers-n'nrnbn-Trava,sila Crimple?.::, 3D-n59: slop?;. - These are very <br />steep areas shallow to interbedded sandstone =_iltston?, .and <br />shale. Usually a sandstone lay?r occurs at the crest of these <br />areas. Sandstone an•d shale outcrop cornpri==-a 10 to Zuq< of the <br />area. South tai-iris slopes are aft?n nearly baYren ~•~h1i? noYth <br />faring slopes are corn~noniy ~=revered ~,~ith oak: Crush and alnon <br />t Yees The 50115 aY? nOn~=31Ca Y?OUS and n?Utl'3 i bUY TaCe 13yeYS <br />are channery loans or channery clay learns. Much of the very Steep <br />side Slopes are anderiain by weathered Shale and have a silty clay <br />loam subsoil. tJarro~., loamy valleys are included within these <br />aYe35 <br />1~]E LOUr/leY S-PY let 3-r'01't I_.O111nS I. O17~pla;.•, c }O Pc% 510pe5. - AbOUt b5~ <br />of the area is shaiio~•; (less than~0" to lot?rbedded sandstone and <br />shaiei and has a Very channerv loam surfa~.e layer. These shallow <br />sails have clay loam 5cbsoils and are nonr,'careous and neutral <br />throughout. The shallaa stony soils o~.cur on ridges and are <br />easily located by the aGundanc? on pinon trae5. About ZO% of the <br />area is Fnrt Collins ioarro and i5 deep, 4p-=:" or more, to <br />sandstan? nr Sh31e and occurs aiona dra:nways. This deap soil <br />has a 103m Jr 'JeYy Tlne Sand;' IJa17~ SUr Tare, a C13V 103m SLLb 5011 <br />and .s noncaicareous and neutral tc ZJ loco?s or nor?. 4 fern <br />stones are commonly encountered ~n the profile. Jeep 5etls occur <br />in open grassy parl::s. About 15°.e of the .area is ra~.I:: eut~_rop <br />C3F t4idnight Pombo Cornpe:., 35 to 5~1'e slope;. - Thesa sot;; are shallow <br />and ri~oderat?ly ~i??p, il] to 40 inches, to w?ath?red sha??. Te.:tur? <br />is clay loam !4hirh _r'3tleS to shalt' clay lnsin ~+ith depth. It is <br />nonraicar?sus and -,=_ctral to about i5 inch?s. Channery stones on <br />the surface Vary from few to many. =011 moisture and plant roots <br />penetrate deep in*~_ r,e frac±ur?d shalt., Eared of int?rbedded <br />sand=_te^;? ~=O'iiipYi== 2CJUL iU p?YC2ni OT the aY?3. <br />PEE Daraol-rueYa-Var;~a, PPie•., 10 to 4"'b ~"=~p_ - These soil=_ are <br />StiallOW lO tO ZJ 1nCneS Or. ridgatOGS, ~dGdar'a[aly deep (ZLI t0 40 <br />inchasi to shale ;us. =ff ~idg?toss, and deep igreater tnan 40 <br />inches) at the base =, steep sid? slopes. wand of Sandstone <br />outcrop occur on bot~ thte rld9? top a',ld Steep side slopes. <br />~urface te;:.tures range from stony loam and learn ~= silty clay <br />