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• 'Itx~ Rcmbo soil is moderately deep and ~,=11 drained. It Toned in s`ony <br />colluvium anal residuum aerLVed cbminantlf :'.ray silts*_one, shale, aid <br />basalt. typically, tr±e sur.°aee layer is channerf silty clay loam 4 inches <br />thick. TI^e u_rper 2C lnc~s cif the subsoil ~s very shalt' and charmer/ sLl*_y <br />clay loan. T.~e lo~.er iC inc!-es is cerr shay sil_v c1=;~ lca~a c~,,.-~ ~-ra~: <br />snail. In scree areas tte surface layer is cla~r_.,_.ilty clay lea^.. 7`.= <br />soil is neutral t!:rcugt;out. <br />ThLS unit is used Sor llvestCCF graz.in.c and •.aildi.i.°e nahLt,t. <br />The ao*_ential slant carnunity a-i this uni` i_= ~~x:rv ~bunta.L; -unir<r, <br />b.l ~] L1ueStem, plr.yon, .:rd tree r+ounta Lrm.ehma,^.y. .~ ::ve rac?A anGUca <br />productirn of a.ir-dry vegetation is i,lu0 xcc-~ rwr acre. I_° t`c <br />COnd LtlOn Of tfle range defer LOruteS, C'af'~L}'_1 Oa,C, pLnvon, and ]un.i7er <br /> Lncrease. :'his unit co~-mcnly is dminated `rv Ca~~hel oak. oteeoce=_s of <br />• sloce limits acce_==_= c ~ 1i.vestoc~ and prmotss over-7razir~ cf t~r_ ___ . <br />slcping aCeaS :a tn2 anlt, i~s9 OC mr:C:7anlC.?1 .rnaU^.'.:1C i)rc.ist.LCi S t =, n~C <br />y^. raCt.l C31, CeC8U5e t'}? SU r'aCS l5 SCOC;% ar1~9 t:^f Sl^"•'' ,9 "r-. ;tac.r:~, <br />7`iis unit is poorly suited to hc^.esire Ce•.'6i:]~d'~?'.t. It Ls iimite.'. by <br />steer ne=_s OL slope, shrinr.-s~r=1i ;c _en*_1:1, a',^ ..i.li'; :: '.~?i th tn. '~Q^r'=C is 1.'1 <br />some areas. <br />Tfi15 ^'ali L'•nLt i5 Ll Ca:%aJ1_L:`! SUt~ia55 1;I?. It L .Lil !CC:-:: ~th111 <br />ran~~2 LCe. <br />• <br />201 <br />