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Alluvial Fans
Where a stream flows out of a steep, narrow mountain valley, the stream suddenly becomes wider and shallower. The water slows down, Here sediments are deposited in an alluvial fan. An alluvial fan is a wide, sloping deposit of sediment formed where a stream leaves a mountain range. As its name suggests, this deposit is shaped like a fan.
An alluvial fan is a fan- or cone-shaped deposit of sediment crossed and built up by streams. They are usually created as flowing water interacts with mountains, hills, or the steep walls of canyons.
An alluvial fan is formed by weathered rocks at the top of the mountain eroding down to the bottom.
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