Article: Greenstone.(Word to the Wise)

Iron is the most abundant chromophore (an element that imparts color to a mineral by its presence in the structure) in the earth. When iron is in its divalent oxidation state ([Fe.sup.2+]), as is found in such minerals as olivine, pyroxenes, amphiboles, chlorites, and epidote, it typically imparts a green color. Exceptions to this do exist and include, for example, almandine, which is colored red by the presence of divalent iron.

Acting as does pigmentation in paint, [Fe.sup.2+]-bearing minerals, even as minor constituents in a rock, can impart a distinct green color, especially when fine grained and highly dispersed. Although many minerals and rocks are green ...

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