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Minerals B-C

Minerals B-C Page of 81 Minerals B-C Text size:minus plus Restore normal size   Mail page  Print this page
Bismuth: A metal with a yellowish or reddish-white color and a lamellar texture that is somewhat harder than lead and scarcely if at all, malleable, being so brittle as to break
easily under the hammer and reducible to powder. It is usually in
foliated granular or arborescent forms, opaque and metallic. It fuses
easily and is useful in the arts and manufactures.
Bismuthinite: Bismuth Tri-Sulphide. A very rare mineral con­taining 81% Bismuth, occurring usually massive with a foliated or fibrous structure. Color lead-gray, with a yellowish or iridescent tarnish. It is used in the manufacture of low fusing alloys, which are used in safety-plugs for boilers and automatic fire sprinklers. Is found in Saxony, Cornwall, and also in Utah, North Carolina and Connecticut.
Bloodstone or Quartz dotted with red spots of Jasper which re-Heliotrope:          semble drops of blood. It has been used to some extent for engraved gems.
Boracite: A mineral composed of Boracic Acid and Magnesia. It is considered an interesting mineral on account of the form and internal structure not corresponding. Its crys­tals have well-defined hextetrahedral symmetry of the isometric sys­tem, and the internal structure is orthorhombic. This is due to the fact that the substance is dimorphous. It is gray, yellow or green, and transparent or translucent.
Boracite is utilized in Europe as a source of Boron compounds, and is found in Stassfurt, Hanover, Holstein, and also in Turkey. It is rare in the United States.
Borax: Sodium Tetraborate. A salt formed by a combination of Boracic Acid with Soda, occurring as crystals, crystalline cement, and as incrustations on the surface of marshes, and on the sands of deserts. This mineral has a white, grayish or bluish color arid a sweet alkaline taste. On exposure to air it loses water and becomes white and opaque. The principal method of occurrence is as a deposit from salt lakes, and as an incrustation on the surfaces of alkaline marshes overlying borax deposits. The original deposits were the result of the evaporation of ancient salt lakes. Until the dis­covery of borax in California, since very early times it has been ob­tained from the salt lakes in Thibet. It is used as an antiseptic, in the arts for soldering brass, and in cosmetics. Borax is especially valu­able as a re-agent in blowpipe analysis; for making colored glazes and enamels for porcelains; and for use in the laundry and bath.
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Morgenthau. Minerals and Cut Stones.
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