Alluvial fans are triangular deposits of sediment called alluvium. These fans occur when fast-moving water is released from the confines of a river or stream bank and then flows over a wider plain.
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Deltas; alluvial fans.
The braided markings on alluvial fans are from erosion caused by braided streams. It is created by the meandering, combining, and separating of the waters as they flow over and around different landforms.
Alluvial fans are when a river slows and deposits sediment on a flatter plain. This would be caused by eroson.
A delta forms when a river empties into a larger body of water. An alluvial fan forms on land where a river emerges from a mountainous area and flows out onto a more gently sloping plain.
Alluvial fans usually created as flowing water interact with mountains. It is a triangle-shaped deposit of sand, gravel and smaller pieces of sediment. There is also a type of alluvial fan that can be found underwater which is the subaqueous fan.
Because they form and look like Fans
Alluvial fans
erosion
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The River Severn does not have an alluvial fan. Rivers that empty into estuaries do not have alluvial fans.
Alluvial fans
base of mountains
In Death Valley, CA
Abyssal Fans, also known as deep-sea fans, underwater deltas, and submarine fans, are underwater structures that look like deltas formed at the end of many large rivers, such as the Nile or Mississippi Rivers. Abyssal fans are also thought of as an underwater version of alluvial fans.
A bajada is an alluvial plain formed at the base of a mountain by the coalescing of several alluvial fans.
In Death Valley, CA
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