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The Soils of Elgin County - Agriculture and Agri-Food Canada

The Soils of Elgin County - Agriculture and Agri-Food Canada

The Soils of Elgin County - Agriculture and Agri-Food Canada

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Organic (OR)Organic l<strong>and</strong> units usually consist <strong>of</strong>depressional wetl<strong>and</strong>s which <strong>of</strong>ten have st<strong>and</strong>ingwater at the surface for long periods <strong>of</strong> time eachyear. <strong>The</strong> organic soils which occur in these l<strong>and</strong>units are very poorly drained <strong>and</strong> variable inmaterial composition <strong>and</strong> thickness . <strong>The</strong>underlying mineral materials are also variable,ranging from coarse textured fine s<strong>and</strong> to veryfine textured silty clay . <strong>The</strong>se l<strong>and</strong> units occuronly in a few small areas in the <strong>County</strong>, <strong>and</strong> theywere not rated for their capability or suitability foragricultural use .soils which may occur in the <strong>of</strong>ten low-lyingfloodplains.<strong>The</strong> slopes <strong>of</strong> the steep side walls generallyexceed 30% . Occasionally the slopes may be lesssteép, especially in valleys with short side slopes .<strong>The</strong> side walls are rated Class 6T to TT forcommon field crops . <strong>The</strong> alluvial terraces <strong>and</strong>floodplains are generally limited in their use foragriculture due to flooding . <strong>The</strong>y are rated Class31 to 51. <strong>The</strong>se l<strong>and</strong> units frequently were mappedwhere the alluvial terrace or floodplain areas werenot large enough to delineate separately on thesoil maps .Scarp (SC)Areas mapped as Scarp l<strong>and</strong> units consist <strong>of</strong>strongly to very steeply sloping cliffs along theshoreline <strong>of</strong> Lake Erie, or they consist <strong>of</strong> similarlysloping river or creek banks adjacent to the majorwater courses which traverse the <strong>County</strong>. <strong>The</strong>l<strong>and</strong> units which occur along the Lake Erieshoreline generally have slopes which are greaterthan 30%. <strong>The</strong>y have been formed by waveerosion which in many places is still active . <strong>The</strong>units which occur along the Thames River <strong>and</strong>major creeks generally tend to have surface slopeswhich are also greater than 30%. Occasionally,however, the surface slopes may range from 15 to30%.<strong>The</strong> soils which occur in these l<strong>and</strong> units arehighly variable in materials <strong>and</strong> drainage.Textures <strong>of</strong> the soil materials range from gravellys<strong>and</strong> to clay. Soil drainage ranges fromimperfectly drained in the clay textured materials,to rapidly drained in the gravelly s<strong>and</strong> texturedmaterials. Areas mapped as this l<strong>and</strong> unit arerated Class 6T to 717 for common field crops.<strong>The</strong>se l<strong>and</strong> units frequently were mapped in areaswhere they occurred adjacent to Alluvium l<strong>and</strong>units which were large enough to delineateseparately on the soil maps.Valley Complex NO<strong>The</strong>se l<strong>and</strong> units consist <strong>of</strong> "U" shaped valleysthat most <strong>of</strong>ten are associated with the ThamesRiver <strong>and</strong> major creeks which traverse the <strong>County</strong>.<strong>The</strong> valleys most <strong>of</strong>ten consist <strong>of</strong> strongly to verysteeply sloping side walls, <strong>and</strong> nearly level alluvialterraces or floodplains. <strong>The</strong> terraces or floodplains<strong>of</strong>ten occupy significant portions <strong>of</strong> the l<strong>and</strong> units.<strong>The</strong> soils which compose the side walls, terraces,or floodplains are quite variable in materials <strong>and</strong>drainage . <strong>The</strong>y range from rapidly drained,coarse textured soils which may occur on thevalley side walls, to poorly drained, clay textured

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