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Alluvial sediment:is clay or silt or gravel carried by rushing streams and deposited where the stream slows down. Alluvial deposition refers to this process.by which alluvium is thus deposited.
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.
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Alluvial fans form where water moving fast (a high energy state) and therefore carrying a lot of sediment of various sizes suddenly slows down (a low energy state) and therefore dumps most of the load it is carrying. They therefore develop where streams issue from canyons onto an adjacent valley floors.
jet streams travel above global winds. might not be a straight forward answer, but its something.
you stink is my answer
herro
alluvial
Frank Anker Engelund has written: 'Investigations of flow in alluvial streams' -- subject(s): Alluvial streams, Hydraulics, Sediment transport
Fluvial soils are associated with streams and rivers. The Alluvial soil category is primarily composed of unconsolidated basin fill that has been deposited and then altered by water.
Alluvial gold is found in the water and reef gold is found in rocks. Reef gold is worth more than alluvial gold. Hope this helps:)
Alluvial soil is clay, silt, or gravel carried by rushing streams and deposited where the stream slows down.
Alluvial sediment:is clay or silt or gravel carried by rushing streams and deposited where the stream slows down. Alluvial deposition refers to this process.by which alluvium is thus deposited.
Alluvial soil comes from the floodplains, streams and rivers; most especially from fertile farmland. It is deposited in the delta or mouth of a river.
· Alluvial fans develop where streams issue from canyons onto adjacent valley floors and deposit sediments derived through the erosion of rocks upstream.
· Alluvial fans develop where streams issue from canyons onto adjacent valley floors and deposit sediments derived through the erosion of rocks upstream.
Where a stream leaves a mountain range is called a Alluvial Fan. An Alluvial Fan is the sediment the streams leave behind as it leaves the range.