Oxidation of iron in ferromagnesian minerals and dissolution of calcite are two examples of mechanical weathering.
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Q71: Rocks always weather chemically before they undergo
Q72: The addition of a small amount of
Q73: Sheeting fractures and exfoliation domes commonly develop
Q74: Thermal cooling, especially of igneous rocks, results
Q77: Release of carbon, nitrogen, and sulphur oxides
Q78: Minerals which undergo oxidation must lose electrons
Q79: Weathering is considered an internal process, because
Q80: The natural decomposition of limestone through chemical
Q81: Pedalfers form more readily than pedocals under
Q86: Sheeting is mainly a process of mechanical
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