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VII.—On the Occurrence of Arenig Shales beneath the Carboniferous Rocks at the Menai Bridge1

Published online by Cambridge University Press:  01 May 2009

Edward Greenly
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Extract

The shore of the Menai Straits on the Carnarvonshire side, nearthe Suspension Bridge, is composed, as is well known, ofsandstones and shales belonging to the Carboniferous Series. Abouta quarter of a mile west of the bridge, however, some fissile, reddishand greenish shales appear on the foreshore, dipping at higherangles than usual. This might easily be ascribed to local disturbance, as a large fault is not far off, though the shale differs somewhat from that which is common in the Carboniferous rocks of the district, a fact which was noticed by Mr. G. H. Morton, who went with me along this part of the section.

Type
Original Articles
Information
Geological Magazine , Volume 5 , Issue 12 , December 1898 , pp. 560 - 562
Copyright
Copyright © Cambridge University Press 1898

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Footnotes

1

Communicated to the British Association, Bristol, 1898.

References

page 560 note 2 The Carboniferous rocks here seen will shortly, I hope, be described by him.

page 561 note 1 The graptolites and other fossils mentioned in this paper have been examined with his usual kindness, by my friend and former colleague, Mr. B. N. Peach, F. R. S.