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Minerals P-R

Minerals P-R Page of 81 Minerals P-R Text size:minus plus Restore normal size   Mail page  Print this page
Rhodolite: A variety of Garnet consisting of two parts Pyrope and one part Almandite. It is pale rose or purple in color and used as a gem stone. Occurs in Macon County,
Georgia
Rhodonite: Pure Manganese Silicate. Silica 46%, Manganese 54%. It occurs in crystals possessing many habits of which the cubical, tabular and columnar are the most common though it also occurs as structureless or granular masses. Color light brownish-red, flesh-red and rose-pink; sometimes greenish, yellowish or even black when impure and from exposure. Fine crys­tals of Rhodonite are found in Sweden, and associated with zinc ores at Franklin, N. J.
The attractive rose-pink color imparted by the manganese, has led to the utilization of this mineral as an ornamental stone. Much of its beauty depends on the matrix effects brought out by the contrast of the deep rose-red Rhodonite with its accompanying minerals. It is essentially a Russian ornamental stone, the raw material being derived from Siberia. The transparent red varieties are used to some extent as a gem stone, the gem material occurring in California and Montana.
Riebeckite: Iron-Sodium Amphibole. This mineral occurs only in embedded prisms showing no terminations. It is black, vitreous and very pleochroic in green or dark
blue tints, that is, exhibiting different colors when viewed in different
directions. It occurs on the Island of Socotra in the Indian Ocean,
also in Corsica and Scotland.
Rock Crystal: A pure, colorless, transparent variety of Quartz, forming distinct crystals, including the variety called "Lake George Diamonds" found in Herki­mer County, New York.
Before glass manufacturing was discovered, Rock Crystal was much used for the carving of transparent objects such as cups, vases, and small ornaments. This art is still practiced in Japan, where the native lapidaries fashion wonderfully symmetrical polished spheres. Rock Crystal is also cut into brilliants, which when set in cheap jew­elry are more durable and brilliant than glass-imitation diamonds. It is also made into faceted beads and pendants.
Roepperite: Iron-Manganese-Zinc Chrysolite. It occurs in large coarse crystals, orthorhombic in habit. Color when fresh, pale yellow; when weathered, dark green to
black. Slightly magnetic. Occurs with Willemite, Franklinite, and
Spinel at Sterling Hill and FranLlin Furnace, N. J.
FIFTY-NINE
Minerals P-R Page of 81 Minerals P-R
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