Hostname: page-component-78c5997874-g7gxr Total loading time: 0 Render date: 2024-11-05T11:18:29.199Z Has data issue: false hasContentIssue false

VII.—On the occurrence of Sillimanite Gneisses in Central Anglesey1

Published online by Cambridge University Press:  01 May 2009

Extract

In the course of some traverses of the central region of Anglesey recently made, preparatory to mapping it out in detail, I observed a few facts which, in spite of the evident complexity of the structures, can, I think, be safely described before completion of the map, and are of some interest in connection with other recent researches in gneissose areas.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1896

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.)

Footnotes

1

An abstract of this paper was read before the British Association, Liverpool, September, 1896.

References

1 In the recognition of these peculiar modes of granitic injection will, I think, be found a reconciliation of the conflicting views that have been held as to the intrusive or “interbedded” character of the granite. I should like also to draw attention to the very vivid and faithful description of these phenomena by Sir A. C. Ramsay (“Geol. North Wales,” ed. 2, p. 243).