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9 Cards in this Set
- Front
- Back
deposition occurs
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when a streams carrying capasity lowers
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a streams lowering carrying capasity
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is usually a result of volume or velocity
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a streams carrying capasity is always
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changing
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when a streams carrying capasity declines
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-some of the streams load stops moving
-and enough sediment is droped off |
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very fine textured materials
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remain suspended indefinately
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Alluvium
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accumulations of stream deposits
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Alluvium is frequently found
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along stream banks and along floors
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alluvium causes soil at the floor of streams
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to be quite fertile
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the carrying capasity is more likely to exceed @
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-inside bends of a stram
-places where channels widen -lower reaches of some streams (especially where water empties into other bodies of water) -behind dams and resivours |