BIPYRAMIDAL CLASS

(Parallel-faced hemihedral).

The elements of symmetry are a tetrad axis with a plane perpendicular

to it, and a centre of symmetry. The simple forms are the same here as

in the holosymmetric class, except the prism {hko}, which has only

four faces, and the bipyramid {hkl}, which has eight faces and is

distinguished as a "tetragonal pyramid of the third order."

[Illustration: FIG. 52.--Crystal of Chalcopyrite.]

[Illustration: FIG. 53.--Crystal of Fergusonite.]

Fig. 53 shows a combination of a tetragonal prism of the first order

with a tetragonal bipyramid of the third order and the basal pinacoid,

and represents a crystal of fergusonite. Scheelite (q.v.), scapolite

(q.v.), and erythrite (C4H10O4) also crystallize in this class.

Encyclopaedia Britannica, 11th Edition, "Crocoite" to "Cuba" Volume 7, Slice 7 · 第 54 / 96 题