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Aragonite |
A mineral form of crystalline calcium carbonate;
dimorphic with calcite.
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Azurite |
A deep blue semiprecious stone that is composed of hydrated
copper carbonate. |
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Barite |
A yellow, white, or colorless crystalline
mineral of barium sulfate, that is the chief source of barium chemicals. |
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Calcite |
Calcite is a common mineral consisting of crystallized
calcium carbonate, a major constituent of limestone.
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Cinnabar |
A heavy reddish mineral consisting of mercuric sulfide;
the chief source of mercury.
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Epidote |
A mineral, commonly of a yellowish green (pistachio)
color, occurring granular, massive, columnar, and in monoclinic crystals.
It is a silicate of alumina, lime, and oxide of iron, or manganese.
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Fluorite |
A soft mineral (calcium fluoride) that is fluorescent in ultraviolet
light. It is the chief source of fluorine.
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Orpiment |
A yellow mineral occuring in conjunction with realgar;
an ore of arsenic.
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Pyrite |
A very common brass-yellow mineral, iron disulfide, with a metallic
luster, burned to sulfur dioxide in the manufacture of sulfuric acid:
chemically similar to marcasite, but crystallizing in the isometric
system. |
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Realgar |
A rare soft orange mineral consisting of arsenic sulphide; an important
ore of arsenic.
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Sphalerite |
An ore that is the chief source of zinc; consists
largely of zinc sulfide in crystalline form.
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Stalactite |
A cylinder of calcium carbonate hanging from the roof of a limestone
cave. |
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Stalagmite |
A cylinder of calcium carbonate projecting upward from the floor
of a limestone cave. |
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Stibnite |
A mineral that consists of the trisulfide of antimony and occurs
in orthorhombic lead-gray crystals of metallic luster or in massive
form. |
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