alluvial fan
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Large alluvial fan in the Taklimakan
Desert, Xinjiang Province, China
Image source: USGS Landsat Project
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A generally fan-shaped area of alluvium
(water-borne sediment) deposited by a river when it reaches a plain on lower
ground, and the speed of flow of the water is abruptly reduced. sand,
gravel, and silt
are the main constituents of the alluvium, with the coarser material deposited
near the head of the fan. Organic matter is also transported, making the
soil highly fertile. Valuable minerals such as cassiterite
(tin ore, SnO2), diamonds, gold,
and platinum are often found in alluvial
fans. Related entry
• delta
Related category
• GEOLOGY
AND PLANETARY SCIENCE Source: U.S.
Geological Survey
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