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How does the rate of rock weathering in dry climates compare to the rate in humid regions ?

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Answered 2 years ago
Answered 2 years ago

In desert regions much of the weathered debris consists of unaltered rock and mineral fragments. These are the result of mechanical weathering processes. Rock weathering of any type is greatly reduced because of the lack of moisture and the scarcity of organic acids from decaying plants. Over long periods of time, clays and thin soils do form, and many iron-bearing silicate minerals oxidize, producing the rust-colored stain that tints some desert landscapes. In humid regions there is more vegetation that influence chemical weathering on a much larger scale.

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