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Ch. 1: Form of Minerals

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26                       A PRACTICAL TREATISE ON GEMS.
The derivation of forms is -that process by which, from one form chosen for the purpose, and considered as the type—the fundamental or primary form—all the other forms of a system may be produced, according to fixed prin­ciples or general laws. In order to understand this process or method of derivation, the student should keep in mind that the position of any plane is fixed when the positions of any three points in it, not all in one straight line, are known. To determine the position, therefore, of the face of a crystal, it is only necessary to know the distance of three points in it from the centre of the crystal, or the points in which the face or its supposed extension would in­tersect the three axes of the crystal. The portion of the axes between this point and the centre are named parame­ters, and the position of the face is sufficiently known wyhen the relative length or proportion of these parameters is ascertained. When the position of one face of a simple form is thus fixed or described, all the other faces are in like manner fixed, since they are all equal and similar, and all intersect the axes in a uniform manner; and the expres­sion which marks or describes one face, marks and describes the whole figure.
The octahedron is generally adopted as the primary or fundamental form of the tesseral system, and distinguished by the first letter of the name, O. Its faces cut the half axes at equal distances from the centre ; so that these semi-axes, or the parameters of the faces, have to each other the proportion 1:1:1. In order to derive the other forms from the octahedron, the following construction is em­ployed. The numbers refer to the descriptions above.
Suppose a plane so placed in each angle of the octahe­dron as to be vertical to the axis passing thi-ough that angle and consequently parallel to the two other axes (or to cut them at an infinite distance =00); then the hexa-
Ch. 1: Form of Minerals Page of 515 Ch. 1: Form of Minerals
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