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Colluvium |
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colluvium [kə′lü·vē·əm]
(geology) Loose, incoherent deposits at the foot of a slope or cliff, brought there principally by gravity. Colluvium fragmental material accumulating on mountain slopes or at the foot of slopes owing to displacement from higher areas by gravity (talus, creep, and slides) or the movement of thawing, water-saturated products of weathering in areas of permafrost. Want to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit the webmaster's page for free fun content. |
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