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Mg2(CO3)(HBO3).5H2O
Monoclinic
Canavesite, a magnesium carbonate borate hydrate mineral, occurs as white sprays of tiny mm-sized crystals on sheared red-willemite ore from Sterling Hill; it has not been reported from Franklin.
Verification was by X-ray diffraction, and nothing more is known of the occurrence. The fluorescence in longwave ultraviolet is violet (pers. comm. R. C. Bostwick).
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| Copyright © 1995 by Pete J. Dunn |
Website
by Herb Yeates
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Link
to homepage
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This
page created: January 11, 2001 |
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