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<br />'r .'~ <br /> <br />"111 <br />,,' <br />",1 <br />, I <br />'ij <br />'i(_ <br />,I. <br /> <br />, f'\ <br />-"Ii <br />f~ <br />At <br />fli! <br />t."" <br />t :.~ <br />}i, <br />J :~ <br />f - t'~- <br />!~t <br />~ , <br />tit'" <br />~ .. <br /> <br />I~.~ <br />~I <br />'.f;i <br />i l:~ <br />iJ~ <br />t '" <br />~' ~:'f <br />1io ,:,~ <br />ih~ <br />ii,~ <br />t l~. <br />U~ <br />J :'i;, <br />, .i'$ <br />~"1 <br />I ;~ <br />~ " <br />~ If <br />H.t <br />! :f,l <br />. 'r,'J:: <br />,,0' <br />H <br />n~ <br />"I.I.. <br />' . <br />,. <br />I' <br />~ '-' <br />~ (. . <br />U <br />" <br />t. <br />~,,: <br />t'J <br />~' <br /> <br />.lr.r.'.:.~ <br />.ll <br />F~) <br />t;it <br />i ~t, <br /> <br />l'l'j <br />.:~ <br />~, <br />;:.:-i <br /> <br /> <br />I\.r~:'..l, <br />'-~ - <br />.. <br />~ T''''' <br />~;l <br />.' ':1 <br />:! '~\4 <br />I" Pi <br />'~r <br /> <br />0:)0934 <br /> <br />. <br /> <br />C3lD - - - C3l clay loam, 5 to 20% slopes. Shallow, 0 to <br /> <br />20 inches to fractured shale. <br /> <br />It is noncalcareous and <br /> <br />mildly alkaline at the surface and becomes moderately <br /> <br />alkaline with depth. <br /> <br />Above the fract~red shale tex- <br /> <br />ture is loam or light clay loam, <br /> <br />In most places <br /> <br />water and tree roots penetrate deep into the fractured <br /> <br />shale. <br /> <br />If these areas are irrigated some seepage will <br /> <br />occur. <br /> <br />GfE Scholle Association, steep. This mapping unit <br /> <br />comprises deep moderately sandy soils intermixed with <br /> <br />. <br /> <br />gravelly and cobbly sandy loarns. They are noncalcareous <br /> <br />and neutral to about 15 inches. A zone of chalky lime <br /> <br />occurs between 20 and 40 inches. The surface layer <br /> <br />consists of pockets of loa:m, stony loam and gravelly <br /> <br />loam. <br /> <br />In small grassy parks on ridge tops and along <br /> <br />drainways small areas of Capulin loam are included. <br /> <br />Capulin soils have a clay loam subsoil and are moder- <br /> <br />ately deep and deep to gravelly and stony loam. These <br /> <br />areas are commonly used as a source of gravel. <br /> <br />. <br /> <br />15 <br /> <br />-'~~~ . <br /> <br />.;..,.. \t~ ..it.i_;.~ __*,~, ..-'" .d.~. ._ ,.t.i .,ioI.~._..II <br /> <br />. ~.. .,_i!Ol'~'" .<il^ l'''~' ....~itJ.,~ 1(.;~ <br />