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V.—Note on the occurrence of Scorodite, Pharmacosiderite and Olivenite in Greenstone at Terras Mine, St. Stephens

Published online by Cambridge University Press:  14 March 2018

Extract

At Terras mine there is an interesting junction of a well-marked tin-bearing elvan, whose course is about north and south, with a bed of greenstone, whose general bearing is nearly east and west. Near the junction, a few years since, a shaft was sunk 40 fathoms deep for the purpose of working a tin lode which was believed to cross the elvan just refered to at that point. At a depth of about 10 fathoms the bed of greenstone was met with, and it continued for 6 fathoms in depth in a very hard state, but from thence to the bottom of shaft it was much softer.

The rock is one of the hardest and toughest I have ever come across. Ordinarily it is composed of a fine-grained mixture of hornblende and silica, but it contains numerous narrow cavities or partial fissures, which near the shaft in question are often studded over or lined with small crystals of the three arseniates mentioned above.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1876

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References

* This is the greenstone referred to by Mr. J. A. Phillips, in his paper recently read to the Geological Society, Vol. xxxii., Part 2, p. 175. Mr. Phillips gives its analysis as follows :—

My attention was first called to this locality for scorodite and pharmaco. siderite in 1872, by Mr. T. Forrester Matthews, of St. Austell. The Olivenite I have discovered recently.