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Ch. 3: Crystalline Structure Gemstones

Ch. 3: Crystalline Structure Gemstones Page of 118 Ch. 3: Crystalline Structure Gemstones Text size:minus plus Restore normal size   Mail page  Print this page
CRYSTALLINE STRUCTURE                    15
This is not so laborious a matter as would appear, for if we take a substance which crystallises in a cube we find it is possible to draw nine symmetrical planes, these being called " planes of symmetry," the intersections of one or more of which planes being called "axes of symmetry." So that iti the nine planes of symmetry of the cube we get three axes, each running through to the opposite side of the cube. One will be through the centre of a face to the opposite face ; a second will be through the centre of one edge diagonally ; the third will lie found in a line running diagonally from one point to its opposite. On turning the cube on these three axes—as, for example, a long needle running through a cube of soap—we shall find that four of the six identical faces of the cube are exposed to view during each revolution of the cube on the needle or axis.
These faces are not necessarily, or always, planes, or flat, strictly speaking, but are often more or less curved, according to the shape of the crystal, taking certain char­acteristic forms, such as the square, various forms of tri­angles, the rectangle, etc., and though the crystals may be a combination of several forms, all the faces of any particular form are similar.
All the crystals at present known exhibit differences in their planes, axes and lines of symmetry, and on care­ful comparison many of them are found to have some features in common : so that when they are sorted out it is seen that they are capable of being classified into thirty-three groups. Many of these groups are analogous, so that on analysing them still further we find that all the known crystals may be classed in six separate systems
Ch. 3: Crystalline Structure Gemstones Page of 118 Ch. 3: Crystalline Structure Gemstones
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