which is a deposition of river sediment along the foot hills
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Alluvial fans have gentler slopes than the cones. Alluvial cones are formed when the slope of hill or mountain front through which the stream descends is steep (fig. 18.15) so that debris collect at the foot of the hills. ... Secondly, the alluvial fans grow in height because of gradual deposition of debris upon debris.
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Depositional landforms are the visible evidence of processes that have deposited sediments or rocks after they were transported by flowing ice or water, wind or gravity. Examples include beaches, deltas, glacial moraines, sand dunes and salt domes.
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