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Minerals D-G

Minerals D-G Page of 81 Minerals D-G Text size:minus plus Restore normal size   Mail page  Print this page
Dolomite: Carbonate of Calcium and Magnesium. Calcium Car­bonate 54%, Magnesium Carbonate 46%. This min­eral is a form of Calcite and is used for many of the same purposes. Much of the common white marble is Dolomite. It is white, reddish or greenish-white, occurring in crystals and in all the forms characteristic of calcite except the fibrous. Its streak is always white, it is transparent or translucent, and is largely employed as building and ornamental stone, massive dolomites being especially deirable as building material. It is found in Switzerland, Mexico, England, also in Vermont, Hoboken, N. J., Niagara Falls, Joplin, Mo., and North Carolina.
Domeykite: A Copper Arsenide. Arsenic 28.3%, Copper 71.7%. Occurs massive and disseminated, color tin-white to steel-gray, becoming covered with a yellow or brown tarnish when exposed to the air. It occurs principally in Chile and is named after the Chilean mineralogist, Domeyko. It also oc­curs in the Lake Superior regions and in California and Mexico.
Dyskrasite: Silver Antimonide. Comparatively rare mineral and composition doubtful on account of the difficulty in obtaining pure material for analyses. Occurs in foli­ated granular and structureless masses; twinning frequent, yielding star-shaped aggregates. This mineral, which is a good conductor of electricity, has a silver-white color and streak, but its exposed surfaces are often tarnished yellow or black. It appears principally in the silver mines of Central Europe, especially at Baden and Harz, and also at Copiapo, Chile.
Ecdemite: Arsenate. Arsenic 12.1%. Occurs in crystals, mas­sive, coarsely foliated or granular. Color bright yellow to green. Translucent in thin splinters. Found at
Langban and Pajsberg, Sweden and Lake Valley, Mexico.
Electrum: An alloy of Gold and Silver. Gold containing silver
to a proportion of 20%. The word in Greek means
amber, and its use for this alloy is probably because of
the pale yellow color. This amber-colored alloy of gold and silver
was used by the ancient Greeks for coins, (see Gold).
Embolite: A grayish-green mineral containing both chloride and
bromide of Silver. The percentage varies in different
specimens, according to the color, the deeper green
colors containing the larger proportion of bromide. Abundant in
Chile, constituting the principal silver ore of the Chanarcillo Mines;
Twenty-five
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