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The chemical formula of mineral Bicchulite is indicated Ca2Al2SiO6(OH)2. Mineral Bicchulite is usually found occuring in skarns in limestones, formed through alteration of gehlenite subjected to later retrograde hydration reactions. Mineral Bicchulite is usually found occuring at its type of locality at Fuka, near Bicchu, Okayama Prefecture, and in the Akagane mine, Iwate Prefecture, Japan. Mineral Bicchulite is known to crystallize in the isometric system of crystal formation. In optical mineralogy, this isometric crystal system comprises crystals having three axes, all of which are perpendicular to one another and all are found equal in lengths.

            Mineral Bicchulite is usually found colorless in hand sample. The specific gravity measure of mineral Bicchulite is usually found 2.75 grams per cubic centimeters. Most crytals of mineral Bicchulite are transparent in appearance. It is also most commonly found leaving a white streak when rubbed on a white porcelain streak plate. Mineral Bicchulite is found to be isotropic when evaluated closely under polarizing microscope used in the field of optical mineralogy. Mineral Bicchulite is found to non-radioactive after chemical evaluation.



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Friday, November 26th, 2010 at 3:44 pm
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Optical Mineralogy
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