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<br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />~ <br />s:.r..~_ <br />- <br />- <br /> <br />...- ~ <br /> <br />I <br /> <br />-,-.-.", ... <br />'~ &~'-"""""--~'--'- <br /> <br />..- <br /> <br />.....,. <br />- ~ <br /> <br />- <br /> <br />- <br /> <br />":J <br /> <br />.~ <br /> <br />....,.~.!J:-~~ .'l; <br />- ....-- <br /> <br />.. <br />~ <br /> <br />I <br /> <br />- <br /> <br />'- <br /> <br />-t~ -'~ <br />~~'J..1i1 <br />~-,.., <br />~-.r.." .; <br />,.._.~.z""'~ .~ <br />,~...,~. <br />".'-"-''".;''k,(. <br />... n~l_00:0.t'.f" <br />~/.:\'};"'ftJ'::'r;! <br />,...~~ ~ , <br />, "..1.. <br />.~... <br />.....' <br />... \'"""j <br /> <br />f~ <br /> <br />I <br /> <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Irrigated hay meadov <br />(Soil Mapping Unit 4) <br /> <br />I <br /> <br />Parent materials for soils of unit 4 are represented by a wide variety <br />of materials. Bottomland and stream terrace soils have formed in <br />mixed alluvial deposits. Large areas of wind blown loamy and silty <br />materials. along with gravelly and cobbly outwash, exist within the <br />unit delineations. They are more widespread here than in the other <br />8 units shown on the general soil map. At many places loamy and <br />gravelly materials mantle residual clayey shales to depths of 4 to 10 <br />feet. Shales where not covered have also furnished residual and <br />reworked parent materials. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Surface soil layers are brown or grayish brown and have <br />organic matter content that ranges from 1 to 3 percent. <br />range from sandy loam to clay loam. <br /> <br />a moderate <br />Textures <br /> <br />I <br /> <br />I <br /> <br />Subsoils are permeable and usually more clayey than surface layers. <br />Sandy clay loams, silty clay loams and clay loams are most extensive. <br /> <br />I <br /> <br />I <br /> <br />. 20 . <br /> <br />I <br />