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Density Currents in connection with the problem of Submarine Canyons

Published online by Cambridge University Press:  01 May 2009

Ph. H. Kuenen
Ph. H. Kuenen
Affiliation:
Groningen, Holland.
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Extract

The investigation of submarine canyons has been actively pursued in the United States of latter years, principally due to the activities of F. P. Shepard. The Coast and Geodetic Survey has mapped a large number of these interesting chasms, both along the Atlantic and Pacific continental slopes, by sonic soundings; Shepard himself added data by soundings and dredgings along the Californian coast; Stetson performed current measurements, dredgings, and sampling in the canyons off the east coast. The number of data is steadily increasing in the United States, and it is to be hoped other nations will also become active, for much still remains to be learned before a comprehensive view of the many-sided problem can be obtained.

Type
Original Articles
Information
Geological Magazine , Volume 75 , Issue 6 , June 1938 , pp. 241 - 249
Copyright
Copyright © Cambridge University Press 1938

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References

BIBLIOGRAPHY

(1)Daly, R. A., Origin of submarine “canyons”, Amer. Journ. Sci., xxxi, 1936, pp. 401–420.CrossRefGoogle Scholar
(2)Eakin, H. M., Silting of reservoirs, U.S. Dep. Agriculture, Techn. Bull. 524, 1936.Google Scholar
(3)Grover, N. G., and Howard, Ch. L., The passage of turbid water through Lake Mead, Proc. Amer. Soc. Civil Engineers, 04, 1937.Google Scholar
(4)Hess, H. H., The Navy Princeton gravity expedition to the West Indies, in 1932, U.S. Hydrogr. Office, 1933.Google Scholar
(5)Kuenen, Ph. H., Experiments in connection with Daly's hypothesis on the formation of submarine canyons, Leidsche Geol. Mededeelingen, 8, 1937, pp. 327–351.Google Scholar
(6)Shepard, F. P., Submarine valleys, Geogr. Review, xxiii, 1933, pp. 77–89.CrossRefGoogle Scholar
(7)Shepard, F. P., American submarine canyons, Scottish Geogr. Mag., 1934, pp. 212–18.CrossRefGoogle Scholar
(8)Shepard, F. P., Canyons off the New England coast, Amer. Journ. Sci., xxvii, 1934, pp. 24–36.CrossRefGoogle Scholar
(9)Shepard, F. P., Submarine canyons of the American coasts, Zeitschr. f. Geomorph., ix, 1935, pp. 99–105.Google Scholar
(10)Shepard, F. P., The underlying causes of submarine canyons, Proc. Nat. Acad. Sci., xxii, 1936, pp. 496–502.CrossRefGoogle Scholar
(11)Shepard, F. P., Continued exploration of California submarine canyons, Trans. Amer. Geoph. Union, 1936, pp. 221–3.Google Scholar
(12)Shepard, F. P., Daly's submarine canyon hypothesis, Amer. Journ. Sci., xxxiii, 1937, pp. 369–379.CrossRefGoogle Scholar
(13)Shepard, F. P., “Salt” domes related to Mississippi submarine trough, Bull. Geol. Soc. Amer., xlviii, 1937, pp. 1349–1362.CrossRefGoogle Scholar
(14)Shepard, F. P., Shifting bottom in submarine canyon heads, Science, lxxxvi, 1937, pp. 522–3.CrossRefGoogle Scholar
(15)Stetson, H. C., Geology and Palaeontology of the Georges Bank canyons, Part I, Geology, Bull. Geol. Soc. Amer., xlvii, 1936, pp. 339–366.CrossRefGoogle Scholar
(16)Stetson, H. C., Dredge-samples from the submarine canyons between the Hudson Gorge and Chesapeake Bay, Trans. Amer. Geoph. Union, 1936, pp. 223–5.Google Scholar
(17)Stetson, H. C., Current-measurements in the Georges Bank canyons, Trans. Amer. Geoph. Union, 1937, pp. 216–19.Google Scholar
(18)Stetson, H. C., and Smith, J. F., Behaviour of suspension currents and mud slides on the continental slope, Amer. Journ. Sci., xxxv, 1938, pp. 1–13.CrossRefGoogle Scholar