Chrysoprase results from the deep weathering or ultramafic ophiolite rocks.
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Deep weathering can occur in cooler climates, but over longer periods of time.
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Saprolites form in the lower zones of soil profiles and represent deep weathering of the bedrock surface.
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Deep weathering of the crust over many millions of years leached chemicals out of the rock, leaving Australian soils deficient in nutrients, particularly phosphorus.
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Deep weathering causes the formation of many secondary and supergene ores & ndash; bauxite, iron ores, saprolitic gold, supergene copper, uranium and heavy minerals in residual accumulations.
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