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<br />Weber Canon, but. in !/l1ther cllsa tl1ay take wator slowly, do not. <br /> <br />drein Mslly, and tend to becOll1e atrongly elltaline, even to the <br /> <br />;Jointer non-j)rodllct1on. Baing i1ne~y divided tbey do not <br /> <br /> <br />heudle 688111 end tend to blllte when irrigated. 1:hay are de- <br /> <br />riv::;d i'rubI tho llicncos 5OO1eB. In the r1ver bed end creek <br /> <br />bottoms, this soil is 6enerelly1n peature, but where it hss <br />better drdnage it 10 cultivated. When well farmed, it produces <br />gOQd Cl'Opll. <br /> <br />lbe two types of salls already described are tlis <br /> <br />better ones of the project end cover the ~eater part of the <br /> <br />erell, c.nd when they eUllt in good depth erc very productive. <br />The remainder of the &re" ill mnde up of.'ecnttered treetl> at <br /> <br />residual BOUll. <br /> <br />The rellidual sandstone 6011a occur e t tlle extreme <br /> <br />l:lOllthern end northern ends of.' the Mancoe Valley, and ere re- <br /> <br />cognized ~ their sandy texture end their color wh1ch runs <br /> <br />from greyillD. 111h1 te to a T\1f;ty brown. i'ib.1J.e free 1.'1'0111 p.ll(a1i <br /> <br />end generally ell drained, !I1lloh of this s011 ie too shallow <br /> <br />for good ferming. A few seeped ereee occur in tllis type due <br />to sll.l!.llow e011 depth and poor IlUbllOll cond1tions. Ibey USIl- <br /> <br />8..l1y contain little organic DlI\tter. <br /> <br />Reeidllol saale solls ere ullually /!,I'e., to blue &1'81 &nd <br />of 1\ very heovy texture, tu!ving been formed from the l4ancoe <br /> <br />1.,"" <br />1.: <br />X> <br /> <br />6heles. TIley occur in I!. number of roundedknollE nnd r1dges <br /> <br />24 <br />