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PRECIOUS STONES
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or trimetric, monoclinic, and triclinic, of which are the alex­andrite, andalusite, cat's-eye, chrysoberyl, hiddenite, labrador-ite, malachite, moonstone, olivine, sphene, and sunstone.
These forms of crystallization are not often clearly de­fined, and are generally rendered difficult to recognize in the stone as it is found, by the modifications occasioned by the conditions surrounding it during existence. The natural form of the diamond, for instance, is that of two four-sided pyramids, united at their bases, or octahedron, but there are many outward variations. It is also commonly found as a rhombic dodecahedron, bounded by twelve lozenge-shaped faces or rhombs. Sometimes it is found as a six-faced octa­hedron, and as the faces are generally more or less curved, the forty-eight faces make it almost spherical. It has been found quite globular in form, upon the surface of which not the slightest appearance of a natural facet could be dis­covered. So also with the ruby: although it is naturally a six-sided prism, it is usually found as a rolled fragment, become so by the processes which released and transported it from the matrix in which it was born. Though harder than the surrounding elements through which it ground its way to discovery during the centuries of its existence, like all other things, the ruby seldom escapes the hand of time scatheless; its own angles become rounded, its rough places are made smooth, the outward features of its crystallization are worn away, and the crystal emerges as a rolled pebble, worn by softer opponents, as a rock is worn away by water.
The amorphous are those found in veins within a matrix. Of these are the opal, turquoise, and obsidian.
Many precious stones have a grain or cleavage, along the lines of which they can be split as wood is; and, as with woods, the cleavage is much more perfect in some than in others. It is for this reason that hard stones sometimes break so easily.
Except in a few cases, the fracture, or break across the