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Ch. 30: Garnet

Ch. 29: Staurolite Page of 252 Ch. 30: Garnet Text size:minusplusRestore normal size  Mail page Print this page
GARNET
This mineral exhibits many varieties of color and of composition. The color probably most often thought of in connection with it is dark red, but it would be a mistake to suppose this the only color which it may manifest. Green, red, rose, and brown are other colors which garnet transparent enough to be used as gems exhibits, while among opaque garnets may be found black and many varieties of the shades above mentioned.
These variations of color are more or less connected with differences of composition which it may be well first of all to consider. Garnet as a mineral is a silicate. United with silica the element most commonly occurring is aluminum. If calcium be united with these two, the variety of garnet known as grossularite, or essonite, or cinnamon stone, is pro­duced. If magnesium takes the place of calcium, then pyrope is formed. If iron, we have almandite, and if manganese, spessartite. Another variety of garnet, andradite, is composed of calcium and iron in com­bination with silica, and still another, uvarovite, of calcium, chromium, and silica. Though they seem to differ so much in composition, all kinds of garnet crystallize in the same system, and are closely allied in all their properties, so that it is an easy matter to distinguish garnet of any variety from other minerals.
Garnet crystals may be of the twelve-sided form known as dodeca­hedrons, the faces of which have the shape of rhombs; or the twenty-four-sided form, known as trapezohedrons, the faces of which have the shape of trapeziums. Quite as commonly occur crystals which are combina­tions of these two forms, and then exhibit thirty-six faces, as in the crystal
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Ch. 29: Staurolite Page of 252 Ch. 30: Garnet
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