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<br />The Can;,ron series con:,i:;ta of ;;hallow, =tong, immature soils which are
<br />developing in place on the caliche Member of the Ogallala formation.
<br />These soil.; occup; the :a•ecper rihba~ anal knob-like areas wnere tho
<br />caliche material:: are expo:;e:, or arc ver~• near the outface. The caliche
<br />materials are commonl;• cncounierel :it ;eni:h.. of 2 to 1$ inches.
<br />'1'heoe soils are bo:;t, ..ui.i.e, Ln ;~raziri;
<br />,OIL PP,Of~II13:
<br />.surface Soil
<br />0 - 3 incre.:, ;-ray brorni l.o.v:r crnitainin~; m•~n}* caliche fragments.
<br />Calea:•cour, .
<br />Parent irlaterial
<br />3 - ll inchce, ;'.ra;• brnam Lo b~•o;ti la,m contain caliche fragments,
<br />lJnweathere:i Parent t•9aterial
<br />ll inches;, plus; cali:.hc: materixd of the Ogallala formation,
<br />v.ir~inl' ir. .;egret o; cem~tation.
<br />Variations
<br />~~ ~:
<br />The principal variations are: The thiclvie;~ of the surface soils, th9
<br />;lept.h to cali.r.hr, .VUI i .t.one matcri:il.: :v~ 1 the t.opop,raphy, 'Phe Qanyot~,. '' . '
<br />soils on .,teep :dope:, include ntirn~, rock c~~Lciron~..
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<br />!4a in Unit:,: :~~' %;•,'
<br />v 1. '.
<br />%vmbol Generalize:: !Jescripti.on _ :. ; • ~:
<br />:,, : .:
<br />52 (i•'i.eld .~I~cet} '1'I:c:,r are: vcr;r .;hallow, stony upland soS$r'6" .; :
<br />have loam;- ,an _l surface soils over7,ying.. a~
<br />liens uarul:,tonc materials at depths of
<br />].H inches. Occupcing the steeper uplEtf~~ ,
<br />area.' with :,ones of 3 to 1$ percart. 4.~,,
<br />53 (r'ita.i .;i~cet) 1'h~;;e are vet;~ sha}1ow, stony upland scri:le
<br />which have ,rrn' loam outface soils over].yiAg
<br />I itri^ rui ~ L~tii~~ ^i:it~rriua..i nt depth rs Of ly t0
<br />1:'. ii ' ~ ~h•, up in • i;ne steeper Upland
<br />~,•„a ,ri l ~ i~.l~,:: or ? t.o 18 percent.
<br />y .i:'4
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<br />.. ~ .. 9 st. '~
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