Online Encyclopedia

WILLEMITE

Online Encyclopedia
Originally appearing in Volume V28, Page 658 of the 1911 Encyclopedia Britannica.
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WILLEMITE  , a

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mineral consisting of
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zinc orthosilicate, Zn2SiO4, crystallizing in the parallel-faced hemihedral class of the
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rhombohedral
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system . Crystals have the form of hexagonal prisms terminated by rhombohedral planes: there are distinct cleavages parallel to the prism-faces and to the
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base . Granular and cleavage masses are of more
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common occurrence . The colour varies considerably, being colourless, white, greenish-yellow, apple-green, flesh-red, &c . The hardness is 52, and the specific gravity 3.9-4.2 . A variety containing much manganese replacing zinc is called " t:roostite." Willemite occurs at Sterling Hill, Sussex county, and Franklin
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Furnace in New Jersey, where it is associated with other zinc ores (
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franklinite and
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zincite) in crystalline
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limestone . It has been found at only a few other localities, one of which is near Liege, and for this reason the mineral was named after William I. of the Nether-lands . Under the influence of. radium radiations, willemite fluoresces with a brilliant green colour . (L . J .

End of Article: WILLEMITE
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FRANCES ELIZABETH WILLARD (1839–1898)
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