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III.—On the Physical Conditions under which the Old Red Sandstone of Scotland was Deposited

Published online by Cambridge University Press:  01 May 2009

Peter Macnair  and
James Reid
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Extract

The physical conditions under which the Old Red Sandstone of Scotland was formed is a subject that has long occupied the attention of many of our leading geologists, from the time of Hugh Miller and Sir Roderick Murchison down to those of the present day. It has been variously regarded as of fresh-water and marine origin, as having been thrown down in lakes and in the open sea, or in inlets of the latter. But as yet the whole matter seems to remain an open question, which the unique physical and palæontological elements of the formation make difficult of solution.

Type
Original Articles
Information
Geological Magazine , Volume 3 , Issue 3 , March 1896 , pp. 106 - 116
Copyright
Copyright © Cambridge University Press 1896

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References

page 107 note 1 “Old Red Sandstone,” 7th edition, p. 53.Google Scholar

page 107 note 2 See “The Old Red Sandstone of Western Europe”—Trans. Roy. Soc. of Edinburgh, vol. xxviii; and “Text Book of Geology.”

page 110 note 1 “Scenery of Scotland,” 2nd edition, p. 141.Google Scholar

page 110 note 2 Trans. Roy. Soc. of Edinburgh, vol. xxviii, p. 383.Google Scholar

page 112 note 1 “Building of the British Isles,” p. 61.

page 113 note 1 “Scenery of Scotland,” 1st and 2nd editions, under the heading ‘Tableland of the Highlands.’

page 115 note 1 Geographical Society's Journal for 1895.

page 116 note 1 British Assoc. Report, 1886.

page 116 note 2 “Elements of Geology,” 3rd edition, p. 435.Google Scholar