1. The Chemical Decomposition of Rocks
They combine with the minerals in rocks to form clays, iron oxides, and salts, which are the endpoints of chemical weathering. ... According to Waugh this process appears to be most active following successive periods of wet and dry weather and is important in forming clay particles. ... Under acidic conditions clay minerals may be produced by the hydrolysis of feldspar. ... Carbonic acid, through its bicarbonate anion, is particularly effective at weathering calcareous rocks like limestone and marble. Generally, when limestone or marble weather via carbonation, all that remains are the insol...
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- Approx Pages: 4
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- Grade Level: Undergraduate