The soils found on mesas, plateaux, and plains are residual soils.
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The residual soils are sandy, almost clay-like and variably deep.
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The residual soils are overlain with aeolian deposits.
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The residual soil was used as foundation and in layers as well above alluvium.
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The embankment dam was located about upstream from the Toccoa Falls and mostly consisted of residual soils and silt.
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Residual soils are soils that develop from their underlying parent rocks and have the same general chemistry as those rocks.
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Within the dam's fill, there were layers of organic residual soil that in one area contained a tree stump.
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Saprolite is a particular example of a residual soil formed from the transformation of granite, metamorphic and other types of bedrock into clay minerals.
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Three fourths of the town is covered by these flatland which may be considered as a broad alluvial plain with recent depositions and residual soils.
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Farther to the north, glacial deposits and wind-deposited loess, a silty soil also associated with the glaciers, are intermingled with the residual soils.
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