Chamyal *, A.S. Khadkikar, J.N. ELSEVIER Sedimentary Geology Sedimentary Geology 107 (1997) 263-279 Sedimentology of the Narmada alluvial fan, western India L.S. Alluvial Fans. Matrix support, a clay content of 3% and clast contact indicate that the clast-support mechanism resulted from a combination of buoyancy and dispersive pressure. An alluvial fan is a build up of river or stream sediments which form a sloping landform, shaped like an open fan or a segment of a cone. Alluvial fan definition is - the alluvial deposit of a stream where it issues from a gorge upon a plain or of a tributary stream at its junction with the main stream. Examples of Alluvial Fan Landforms: Death Valley National Park, California, USA. Exiting the Himalayan foothills onto the level plains, the river itself traverses into India and eventually feeds into the Ganges. It has an area of almost 15000 square kilometers. Aided by the wet climate in the region, the fan spreads over an area of around 15,000 square kilometers. Here are some images of the simulated formation of a coalescing alluvial fan from two sources over a period of approximately 30,000 years, entailing tens of thousands of individual discharge events (this took under a couple of hours of CPU time on a reasonably fast Windows-based computer): An alluvial fan is basically a fan-like structure formed from the mouth of a flattened and spread out stream (it looks like a fan). It has an area of almost 15000 square kilometers. One of the largest and most prominent examples of an alluvial fan is the megafan at the Koshi River in Nepal. See more. A good example would be the ones in Death Valley, California.

Alluvial fan activity near Flaxmill Creek, Makarora East The architecture is dominated by debris-flow deposits (Gms facies). Malik, D.M. The best example of an alluvial fan is the one in Nepal created by the streaming Koshi River. Examples of Alluvial Fan Landforms: Death Valley National Park, California, USA. Alluvial fan definition, a fan-shaped alluvial deposit formed by a stream where its velocity is abruptly decreased, as at the mouth of a ravine or at the foot of a mountain. The Narmada alluvial fan is one of the world's largest, with an axial length of 23 km. Near the mountains south of the Taklamakan Desert in Xinjiang, China lies an alluvial fan 25 miles long and nearly as wide. Flooding on alluvial fans can be damaging as the fans have steeper gradients than river floodplains. Near the mountains south of the Taklamakan Desert in Xinjiang, China lies an alluvial fan 25 miles long and nearly as wide.

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