Calamine
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“Orthohombic, hemimorphic. Crystals usually tabular parallel to the brachypinacoid. They show prism faces and are terminated above usually by a combination of macrodomes and brachydomes and base, and below by a pyramid.” — Ford, 1912
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William E. Ford Dana's Manual of Mineralogy (New York: John Wiley and Sons, Inc, 1912) 261
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