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Ch. 1: Form of Minerals

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FORM OF MINERALS                                    63
duce intersecting macles like the pentagonal dodecahedrons of iron pyrites in fig. 70, and the tetrahedrons of gray-cop-
per or fahlore in fig. VI, a similar formation also occurring ' in the diamond. In macles with inclined axes the two forms almost always unite by a face of the octahedron, and the two individuals are then generally apposed and short­ened in the direction of the twin axis by one half, so that they appear like a crystal that has been divided by a plane parallel to one of its faces, and the two halves turned round on each other by an angle of 180°. In this manner two octahedrons of the spinel, magnetic iron ore, or automolite
(fig. 72), are frequently united. The same law prevails in the intersecting cubes of fluor spar, iron pyrites, and galena,
Ch. 1: Form of Minerals Page of 515 Ch. 1: Form of Minerals
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