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An alluvial fan is a geological feature formed by the deposition of sediment carried by a stream as it emerges from a narrow canyon onto a broader plain. These deposits are typically fan-shaped, with the apex at the canyon mouth and the base extending outwards.12

Alluvial fans are commonly found in arid and semiarid regions, where seasonal rainfall or snowmelt can cause flash floods that transport sediment. The material deposited ranges from coarse gravel near the apex to finer sands and silts towards the base. These features are economically important as they can serve as significant groundwater sources for irrigation and life support, and some cities, like Los Angeles, are built on them.134

A "rock fan" is a similar fan-shaped bedrock surface at the foot of a mountain, which may be covered by a thin layer of alluvium and can be mistaken for an alluvial fan. A "fan delta" is an alluvial fan that merges with a river delta.56

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