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P PPPP r 3 r <br />.fine textured alluvium derived from the upland loess and shale. Silty and <br />clayey alluvium preu0niratoo in - che area adjsaoen'u to the i'latte _rivor but there <br />are minor areas 4r :e,cr soils hove. (ieveslopad on coarse textured or sandy alluvium. <br />Deep and med.tum depth hardianc! soils are found over tho greater ,)art of the up- <br />lands, kx ee brown soils :save oo ve luain or clgsy loam sucx " soils. <br />T. su sod <br />' a <br />are eamaonly slowly permasaul® rand are a heavy alaY loam Ul texturee sdiurs <br />depth soils are found on the stronger slopes tnid core usually under -aid by shale^ <br />or 3ondtstrne. :ylones range from VAO 'til and water erosion is rn <br />Deep airci r. -edium d.er)th sandy soils of the u,.)lands are of miner extent. jhe <br />princip=al arena is .north of Little Ivry Greek and ininediate3ly attest <1P tPso "'Iatte <br />l=iver Valley. 'These brown soils have sandy loam or loamy sand surface textures. <br />The subsoils range from moderately periwcCol r to vo"Y f&Pidly ,P(Ir. :aeable. These <br />soils are uaderlaid principally by sand a:idi su%idstone but sliule may 'he - resent. <br />The slopes range from 5/to 10% and both wind and vrater erosion are evident. <br />moderate € nd severe wind erosion predomi.natee <br />Shallow upland suiis are of minor extent. These brown soila oc=cur principally <br />on tine south slopes burderinl; U Dry 'reek raid alon tho l.r r or intf rnittant <br />tributaries. owall areas occur as knobby points and ridges throughout the <br />uolarui ;. 1hosse soils vary ire ti :eis c .uraoter stic s de= �nd ing upon ' i :�earc�nt <br />Material which ml--y be aaleareous Fra'%rellyr outivas:a ssho.le or sarrdstczto. 'y <br />the surface soils are loams or sandy 10AMs and tho subsoils rsan from slowly <br />to rapidly permeable. Slopes range fron 5%oto 1e,,% and water erosion is :lost <br />evident. There are local areas of severe erosion but mod.erat - o eroslon is domi- <br />nant. <br />