Abstract

1. Chrysoberyl, BeAl 2 O 4 , is analogous in chemical composition to spinel, MgAl 2 O 4 , and the other members of the spinel group, but it bears no resem­blance to them in its crystalline form. The spinels are cubic, and have a very simple structure, which has been analysed by S. Nishikawa and W. H. Bragg, The same type of structure has been discovered in other compounds, Chryso­beryl belongs to the orthorhombic holohedral class, the axial ratios being a : b : c = 0·4707 : 1 : 0·5823. The “ a ” axis is an axis of pseudo-hexagonal symmetry. The angle (011) : (011) is 60° 26', and the ratio of b to c is very nearly √3 : 1 or 1 : 0·577. The crystal twins in a manner very similar to that of aragonite, three individuals interpenetrating so as to form what appears to be a simple hexagonal crystal. The examination of the structure is interesting for two reasons. Firstly, it is curious that it shows such contrast to that of a spinel. Secondly, the axial ratios are almost identical with those of the olivine group of minerals, and are nearly given by the ratio √ ⅔ : 1 : √3/3.

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