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HEMIMORPHIC

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Originally appearing in Volume V07, Page 579 of the 1911 Encyclopedia Britannica.
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HEMIMORPHIC CLASS (Sphenoidal). In this class the only See also:

element of symmetry is a single dyad See also:axis, which is polar in See also:character, being dissimilar at the two ends. The See also:form (0101 perpendicular to the axis of symmetry consists of a single See also:plane or pedion; the parallel See also:face is dissimilar in character and belongs to the pedion {oio1. The pinacoids 1100), See also:tool}, {hol} and (hol} parallel to the axis of symmetry are geometrically the From µ6VOt, single, and KXLVSLP, to incline, since one axis is inclined to the plane of the other two axes, which are at right angles.same in this class as in the See also:holosymmetric class. The remaining forms consist each of only two planes on the same See also:side of the axial plane XOZ and equally_ inclined to the dyad axis (e.g. in fig. 62 the two planes X YZ and X YZ) ; such a See also:wedge-shaped form is some-times called a sphenoid. Fig. 64 shows two crystals of tartaric See also:acid, a a right-handed crystal of dextro-tartaric acid, and b a See also:left-handed crystal of laevotartaric acid. The two crystals are enantiomorphous, i.e. although they have the same interfacial angles they are not superposable, one being the See also:mirror See also:image of the other. Other examples are See also:potassium dextro-tartrate, See also:cane-See also:sugar, See also:milk-sugar, quercite, See also:lithium sulphate (Li2SO4•H20); amongst minerals the only example is the See also:hydrocarbon fichtelite (CbH8).

End of Article: HEMIMORPHIC

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