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The Convection Current Hypothesis of Mountain Building

Published online by Cambridge University Press:  01 May 2009

A. J. Bull
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Extract

IN a previous paper in the Geological Magazine (1) the hypothesis was suggested that mountains might result from the dragging together of sediments and other rocks by a convection current inthe material below the crust. It may be useful to review the present position as to how far this idea has offered an adequate explanation of mountain and other earth structures.

Type
Original Articles
Information
Geological Magazine , Volume 68 , Issue 11 , November 1931 , pp. 495 - 498
Copyright
Copyright © Cambridge University Press 1931

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References

REFERENCES

Bull, A. J., Geol. Mag., LVIII, 1921, 364.CrossRefGoogle Scholar
Bull, A. J., Proc. Geol. Ass., xxxviii, 1927, 145.CrossRefGoogle Scholar
Evans., J. W. Q.J.G.S., 1925, cxvi.Google Scholar
Bull, A. J., Proc. Geol. Ass., xl, 1929, 105.CrossRefGoogle Scholar
Holmes, A., Mining Mag., xl, 1929, 205, 286, 340.Google Scholar
Holmes, A., Trans. Geol. Soc. Glasgow, xviii, part iii, 1928–9, 559.Google Scholar