Hostname: page-component-cd9895bd7-gvvz8 Total loading time: 0 Render date: 2024-12-25T07:21:38.141Z Has data issue: false hasContentIssue false

The Metamorphism of the Carrock Fell Gabbro; with a Note on the Origin of the Sulphide Veins of the Caldbeck Fells

Published online by Cambridge University Press:  01 May 2009

Extract

WITHIN the last two years a cutting has been made at the south-east corner of Carrock Fell, a few yards north of the village of Mosedale, for the purpose of obtaining road-metal. This has opened an interesting section near the margin of the intrusion. The rocks exposed comprise two varieties of gabbro and enclosed Eycott lava. Of the two types of gabbro, that next the lava is of the quartz-bearing variety, exhibiting the prevailing dark-green tint in the hand specimen, and carries large flakes of biotite. This is succeeded by the same type of gabbro, but in a highly metamorphosed condition, at once evident in the hand specimen, which is lighter in colour, primarily owing to the decomposition of the felspars.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1920

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

page 267 note 1 The material taken for analysis was free from calcite.Google Scholar

page 267 note 2 Quart. Journ. Geol. Soc., vol. 1, 1894, p. 323.CrossRefGoogle Scholar

page 268 note 1 Quart. Journ. Geol. Soc., vol. li, 1895, p. 133.Google Scholar

page 268 note 2 Trans. Cumb. and West. Assoc. Lit. and Sci., vol. xv, 18891890, p. 78.Google Scholar

page 268 note 3 Boyschlag, , Vogt, , and Krusch, , “The Deposits of the Useful Minerals and Rocks”: Trans. Truscott, vol. i, 1914, p. 69.Google Scholar