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Minerals S

Minerals S Page of 81 Minerals S Text size:minus plus Restore normal size   Mail page  Print this page
Satin Spar: A fine fibrous, silky variety of either Carbonate or Sulphate of Lime. A fine fibrous variety of Calcite; a silky fibrous variety of Aragonite; and a finely fibrous
variety of Gypsum.
Scapolite: One of a group of tetragonal silicates containing Alumi­nium, Calcium and Sodium, white, or grayish-white in color except when impure, when it is much darker. Occurs in Prussia, Italy and Norway; also in New York, Connecti­cut and Massachusetts.
Scheelite: Calcium Tungstate. Tungsten 80%, Lime 20%. It sometimes contains a little molybdenum in place of some of the tungsten. It occurs in crystals, also in reniform
and granular masses; is white, yellow, brown, greenish or reddish in
color.
This mineral is valued commercially as a source of Tungsten, which is used in the manufacture of tool-steel, electric furnaces and targets for Roentgen Rays. It is employed also as filaments in elec­tric light bulbs and other minor purposes.
It is found in Bohemia, Saxony, Cumberland, England; also in Connecticut, Colorado, Arizona, Nevada, and other places in the United States.
Scolecite: Silica 50%, Alumina 26%, Lime 14%. This mineral occurs in silky fibrous and dense radiating masses, and also in slender crystals, transparent or translucent, in cavities of volcanic rocks and in veins. Crystals have been found on Roman tiles that have been exposed for centuries to the waters of the hot springs at Plombieres, France. It occurs also in Switzerland, Iceland, Scotland and at Table Mountain, Colorado.
Selenite: A transparent crystallized variety of Gypsum, occurring either in distinct crystals or in broad folia, the folia some­times a yard across and transparent throughout. It is usually flexible, yielding a fibrous fracture. Handsome Selenite oc­curs near Lockport, New York, (see Gypsum).
Sepiolite: Hydriated Silicate of Magnesium, (see Meerschaum).
Serpentine: A Magnesium Silicate. Silica 44%, Magnesia 43%.
Sometimes a part of the magnesia is replaced by iron,
giving rise to the many colors of the numerous varieties.
It occurs in crystals, fibrous, foliated and massive, with color greenish,
brownish, white or gray. The variety known as "noble serpentine" is
Sixty-three
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