III.—The Origin and Mode of Formation of the Permian Breccias of the South Devon Coast-Reference-Cited by-同舟云学术

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III.—The Origin and Mode of Formation of the Permian Breccias of the South Devon Coast

Published:1906-07 Issue:7 Volume:3 Page:310-320
ISSN:0016-7568
Container-title:Geological Magazine
language:en
Short-container-title:Geol. Mag.

Author:

Hobson Bernard

Abstract

After visiting in 1905 the excellent exposure of the Permo-Carboniferous Dwyka Conglomerate, containing glacially striated boulders, overlying glacially striated Barberton beds at the foot of Gotshe Mountain in the Vryheid district of Natal, it occurred to me to examine the Permian breccias of the South Devon coast to see whether I could find any evidence of their being of glacial origin.

Publisher

Cambridge University Press (CUP)

Subject

Geology

Reference31 articles.

1. Hobson B. , “Basalts and Andesites of Devonshire, etc.”: Quart. Journ. Geol. Soc., 1892, p. 500.

2. “Report on the Geology of Cornwall, Devon, and West Somerset,” 1839, p. 204.

3. Ussher W. A. E. , Geol. of Torquay: Geol. Survey Mem., 1903, pp. 110, 111.

4. Proc. Geol. Assoc., vol. xvi (1900), p. 434.

Cited by 5 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. The Lower New Red Sandstone of the Crediton Valley;Geological Magazine;1963-04

2. The New Red Sandstone of South Devonshire;Geological Magazine;1948-12

3. Breccias.;Geological Magazine;1928-03

4. The geology of the Torquay district;Proceedings of the Geologists' Association;1928-01

5. The petrography and correlation of the Permian rocks of the Torquay Promontory;Proceedings of the Geologists' Association;1927-01

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