The slopes above streams and rivers are subjected to a variety of processes that cause them to recede and retreat from the river or stream channel. These processes, collectively called mass wasting, can be classified according to rapidity of movement and according to the type of materials that are transported.
ISO Metadata Record
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Slump, Pacific Palisades, Southern California
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Earthflow, Chalet Du Fer, Leysin, Switzerland
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Head of Slump, Black Hills, North Dakota
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Surface subsidence (hydrocompaction) of soils, San Joaquin Valley, California
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Sinking, Coal Mine Collapse, Lafayette, Colorado
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