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22 Friends of the Mississippi River Camp Cozy Park NRMP <br />SOILS <br />Soils vary slightly across the site and are most influenced by interaction with the Elk River. Four <br />specific soil types are present with three of those types attributed to the Elkriver soil series. <br />This series consists of very deep, somewhat poorly and moderately well drained soils that <br />formed in postglacial alluvium consisting of a coarse-loamy mantle and underlying sandy <br />sediments on flood plains. These soils have moderate and moderately rapid permeability in the <br />upper part and rapid permeability in the underlying material. The northwestern forest, <br />northern prairie, southern forest and southern remnant prairie have these fine, sandy loams <br />that are rarely flooded. The eastern and central forest areas that extend to the park’s southern <br />floodplain have fine sandy loams that are occasionally flooded. The floodplain terrace has a <br />more unique soil complex made up of both very poorly drained and poorly drained soils with <br />sandy particle sizes. <br />A summary of soils and their associated characteristics is listed in Table 1 and can be visualized <br />in Figure 7. <br /> <br />Soil formation is the result of the interaction of five soil-forming factors: parent material, <br />climate, organisms, topographic position or slope, and time (Foth 1990). Taken collectively, <br />these factors can help determine the dominant floral and faunal communities that helped form <br />the soils. The predominant soil types which fall into the Elkriver series are all sandy loams which <br />are well-suited to cultivation, and in fact, almost all areas of Elkriver soils are cropped with corn <br />soybeans, and small grains with small areas of native vegetation in prairie grasses. These soils <br />would have been dominated by graminoid vegetation (prairie or savanna) prior to European <br />colonization. Due to the fine, sandy nature of some of the soils, the erosion potential is mostly <br />medium; none of the soil types present have a high erosion potential, though all types are <br />susceptible to some erosion by wind, water, or both. <br /> <br />Table 1. Soils <br />Soil <br />Code Soil Name <br />Percent <br />Slope Acres Soil Family <br />Hydric <br />(yes <br />or no) Drainage <br />771 <br />Elkriver fine <br />sandy loam, <br />rarely <br />flooded 0 to 2 15.1 <br />Coarse-loamy, <br />mixed, superactive, <br />frigid Cumulic <br />Hapludolls N <br />Moderately <br />well drained <br />1255 <br />Elk River fine <br />sandy loam 0 to 2 14.5 <br />Coarse-loamy, <br />mixed, superactive, <br />frigid Cumulic <br />Hapludolls N <br />Somewhat <br />poorly to <br />moderately <br />well-drained <br />1257 <br />Elk River- <br />Molsford <br />complex 0 to 6 14.2 <br />Coarse-loamy, <br />mixed, superactive, <br />frigid Cumulic <br />Hapludolls N <br />Moderately <br />well-drained