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Published byPhilomena Hall Modified over 8 years ago
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SOIL A mixture of rock particles, minerals, decayed organic matter, air, and water. Soil composition depends on the size of the individual particles (gravel, sand, silt, and clay)
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Residual Soil The parent rock weathers, and then the weathered material stays put This type of soil is found in Georgia, Kentucky, and Virginia
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Transported Soil The parent rock weathers, and then the weathered material is moved to a different location An example where this occurs is Michigan, where soil was deposited by glaciers
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Factors of Soil Formation
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Climate The most significant factor controlling soil formation Temperature, wind, and rainfall determine the type of soil that can develop
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Topography Hillsides have shallow soils, while organic material accumulates in valleys and flat areas
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Parent material Depends on the environment and bedrock it came from Coarse soil deposited by water Volcanic soil
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Biological Activity Prairie and fertile farm land is rich in organic matter Decaying organic matter is called humus
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Time As time passes clearer horizons formed. Over thousands of years a soil can be depleted of its minerals
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