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<br />~`r•::~ hill~•rsn~ls „r; on moiuil.:,sn sidaalopos at elevations oi' '7500 to 9600
<br /> feet. 'I'lie e'-^;r:.rr :uu~unl. procil. Cnl.i^n is ••houi: 2? inches, t}ro m^:~n annuol air
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<br />t.~•, .,,.::•.lur~, .is nhnnt 40c'}'., and thrr avera~-.~: ^rost-free pe••iu•i is `,o~+t F.0 daps.
<br /> 1'h•~ r.„il: :.eil nrC'ip.Les t',^ open, p:a~•1;-li.l:o parts of t::n lanrlscapc. It r,ekrs
<br />~, ~ nn nl•:~~~~. .'l, pe.•r,cn+, of t!.e. unit. 'i'ha~Ans;l so'1 n,cnl~ies the,coni""ro S-
<br />,, I'or• •.,L^ I ~• siLinns. IY, msk^.s up nh~, il, 30 ;16^CCtlt or' tha unit. Th•, Anvik
<br />1~ so11 hn : i.h' c're••, .}n,.1- color a:] sn •facq layer.
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<br />i:,^71 T':o rlnvik soil is I,ep ar.~} w; 11 drained. It for^~od in sl luviirm from °
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<br />n~xc I mi~•'~ro leery narrn,i, rru,+,o•-ia's. 1
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<br />~• Tyric;:l Ly the s•rr•Pecu ]ayor is vary do k rrayis?•.-prow: loam nho rt 12
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<br />~.~;,, inc!r;c +:hick. T}:e sabsurfnco is brov.n loan abut 6 inchos thick. °'hc suhsuil ~
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<br />a is -ir it -rupiah-hrrwrn ~•Lne loom rrhont. 24 inchn; thick. The suhstr.,'.um is clay
<br />!~ lu!.r Ch•++: extends bal,,vr GU inches. •
<br />P.~rn,;abilit;~ is mode-ate to muaerately slow. 'r',I'fectivo ro~tinF depth
<br />is 30 t.o ti0 inches and tha available ,ester ca}•acit;: is 0.17 to 0.21 in./in.
<br />5urf~re runoff.' is slow and the erosiur. hazard is stirht. ~
<br />. ~ Ti,o Anso1 so. is deep and yell ~h•a'ned. It formed in alluvi•nn from
<br />~~ mizerl min•erolor;,r parent ria+.erials. 1
<br />T.~picnll~~ the surface luyer is r;rnyis};-hrovrt, loam ob.;ut 12 inches thick.
<br />The su},soil is dark l~rovm cla~~ loam ahuut 74 inches thick. The s~instrat,sn is
<br />+}ark yel.tovris'•:-hrown loam thot. ezten is bolow 1i0 inchos.
<br />"crmreahiLity is m"ierHte to m"•lerately slow. Affective root in r, depth is
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<br />25 {.~• '~, inohos aml tho avnila?,lc vr.~f.o^ r.npncit±~ is U.14 to 0.19 in./in. ,.
<br />,~`^~ &+rf,~-+~ n~nr~f+' ;n slaw and the nrusi'm hazard is sl.iE•ht.
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