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Tabular spessartine crystals in muscovite

Published online by Cambridge University Press:  14 March 2018

Edgar D. Mountain
Affiliation:
Rhodes University College, Grahamstown

Extract

During the course of a survey of the mineral deposits of the area immediately south of the Murchison Range in the NE. Transvaal, a visit was paid to the Union mica mine, one of the only two producing mica mines in South Africa. Interest very soon centred round the occurrence of flattened garnet inclusions in a large number of the mica sheets inspected in the trimming hut. A description has been given by A. L. Hall of the nature of the occurrence of the muscovite, while the geology of the area surrounding the mine is shown in a general way on his map. However, no mention was made of platy garnet crystals; and the Union mine is shown on the map as the Premier mica mines, a name by which it was then known. It is situated on the farm Inyoko (or Inyoka) (24° 8' 25" S., 30° 50' 49" E.) on the western slopes of a ridge overlooking the Sandspruit valley, and lies only two miles from Mica Siding on the Selati Railway, though best approached from Gravelotte by road, a distance about 22 miles.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1938

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References

page 125 note 2 Hall, A. L., Mica in the eastern Transvaal. Mem. Geol. Survey, South Africa, 1920, no. 13. [Min. Abstr. 1–270.]Google Scholar

page 130 note 1 Amer. Inst. Mining and Metall. Engineers, Lindgren volume, 1933. [M.A. 6–3.]

page 131 note 1 English translation by L. J. Spencer, 1912, p. 331.

page 132 note 1 C. Frondel, 1936, vol. 21, p. 777; C. Frondel and G. E. Ashby, 1937, vol. 22, p. 104. [M.A. 6–517, 518.]