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XVI.—The Loss of Heat by Conduction from the Earth's Crust in Britain

Published online by Cambridge University Press:  15 September 2014

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Extract

The object of this paper is to record certain temperatures which were measured in the deep Boreland Bore, near Dysart, in Fife, and to discuss the bearing of these and some other observations on the amount of heat which escapes from the crust, by conduction, in Britain.

Type
Proceedings
Copyright
Copyright © Royal Society of Edinburgh 1940

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References

References to Literature

Anderson, E. M., 1909. “On the Temperature-Gradients of Deep Bores, with special reference to those of the Balfour Bore, Cameron Bridge, Fifeshire,” Trans. Edin. Geol. Soc., vol. ix, part 3, p. 167.CrossRefGoogle Scholar
Anderson, E. M., 1934. “Earth Contraction and Mountain Building (I),Gerlands Beitr. zur Geophys., vol. xlii, p. 133.Google Scholar
Anderson, E. M., 1938. See KENNEDY, W. Q.Google Scholar
Benfield, A. E., 1939. “Terrestrial Heat Flow in Great Britain,Proc. Roy. Soc., A, vol. clxxiii, p. 428.Google Scholar
British Association Committee on Underground Temperatures, 1870. 2nd Report. Brit. Assoc. Report, 1869, p. 176.Google Scholar
British Association Committee on Underground Temperatures, 1871. 3rd Report. Brit. Assoc. Report, 1870, p. 29.Google Scholar
British Association Committee on Underground Temperatures, 1873. 5th Report. Brit. Assoc. Report, 1872, p. 128.Google Scholar
British Association Committee on Thermal Conductivities of Rocks, 1879. 5th Report. Brit. Assoc. Report, 1878, p. 133.Google Scholar
British Association Committee on Thermal Conductivities of Rocks, 1880. 6th Report. Brit. Assoc. Report, 1879, p. 58.Google Scholar
British Association Committee on Thermal Conductivities of Rocks, 1882. Final Report. Brit. Assoc. Report, 1881, p. 126.Google Scholar
British Association Committee on Thermal Conductivities of Rocks (appointed 1934), 1938. Report. Brit. Assoc. Report, 1938, p. 271.Google Scholar
Bullard, E. C., 1939. “Heat Flow in South Africa,Proc. Roy. Soc., A, vol. clxxiii, p. 474.Google Scholar
De Geer, G., 1935. “Dating of Late-Glacial Clay Varves in Scotland,” Proc Roy. Soc. Edin., vol. lv, part 1, p. 23.Google Scholar
Hales, A. L., 1937. “Convection Currents in Geysers,Mon. Not. R. Astr. Soc. Geophys. Suppl., vol. iv, p. 122.Google Scholar
Kennedy, W. Q., and Anderson, E. M., 1938. “Crustal Layers and the Origin of Magmas,” Bull. Volcanol., ser. 2, vol. iii, p. 23.Google Scholar
Krige, L. J., 1939. “Borehole Temperatures in the Transvaal and Orange Free State,” Proc. Roy. Soc., A, vol. clxxiii, p. 450.Google Scholar
Meteorological Office, 1936. “Averages of Temperatures for the British Isles for periods ending 1935.”Google Scholar
North of England Institute of Mining and Mechanical Engineers, 1894. Borings and Sinkings, vol. S–T, p. 162.Google Scholar
Van Orstrand, C. E., 1924. “Temperatures in some Springs and Geysers in Yellowstone National Park,” Journ. Geol., vol. xxxii, p. 194.CrossRefGoogle Scholar
Woodhead, T. W., 1928. “The Forests of Europe and their Development in Post-Glacial Times,” Emp. For. Journ., vol. vii, No. 2.Google Scholar
Wright, W. B., 1937. The Quaternary Ice Age, 2nd ed., p. 452.Google Scholar