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chlorophoenicite.pdf
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Chlorophoenicite is a mineral with the chemical formula (Mn, Mg)3Zn2(AsO4)(OH, O)6, crystallizing in the monoclinic system. It forms stout to acicular prismatic crystals, often with etched and dull terminations, and exhibits a light grayish green color in natural light, turning pink to light purplish red in artificial light. The mineral has a vitreous, silky, or pearly luster, and its optical properties include a biaxial (-) orientation and strong dispersion. Chlorophoenicite occurs in secondary cracks through franklinite ores in a metamorphosed stratiform zinc orebody, and is associated with minerals such as leucophoenicite, hodgkinsonite, and willemite. It is found in Franklin and Sterling Hill, New Jersey, USA, and was named for its distinctive colors in natural and artificial light.

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Description

Chlorophoenicite is a mineral with the chemical formula (Mn, Mg)3Zn2(AsO4)(OH, O)6, crystallizing in the monoclinic system.

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