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A Suggested Origin of Continental Slopes and of Submarine Canyons1

Published online by Cambridge University Press:  01 May 2009

K. O. Emery
K. O. Emery
Affiliation:
(University of Southern California)
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Abstract

Thrusting along a shear plane at the continental margins may result in a temporary up-bulging of the margins above sea-level. During the time of exposure erosion by streams should have incised canyons which now, after isostatic readjustment of the margins, constitute the widely distributed submarine canyons. Known downwarped peneplains below the surface of continental shelves may have been developed on the bulged margins by long continued erosion. The margins may, thus, have served as- sources of some sediments now found on land and believed to have been derived from a seaward direction.

Type
Articles
Information
Geological Magazine , Volume 87 , Issue 2 , April 1950 , pp. 102 - 104
Copyright
Copyright © Cambridge University Press 1950

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Footnotes

1

Contribution of Allan Hancock Foundation.

References

REFERENCES

Ashley, G. H., 1935. Studies in Appalachian Mountain Sculpture. Bull. Geol. Soc. Am., 46, 1395–1436.CrossRefGoogle Scholar
Bullard, E. C., 1936. Gravity Measurements in East Africa. Phil. Trans. Roy. Soc., London, ser. A, ccxxxv, 445–531.Google Scholar
Bullard, E. C., and Gaskell, T. F., 1938. Seismic Methods in Submarine Geology. Nature, 142, no. 3603, 916–17.CrossRefGoogle Scholar
Toit, A. L. Du, 1940. An Hypothesis of Submarine Canyons. Geol. Mag., 77, 395–404.CrossRefGoogle Scholar
Gutenberg, B., and Richter, C. F., 1937. Depth and Geographical Distribution of Deep-Focus Earthquakes. Bull. Geol. Soc. Am., 49, 249–288.CrossRefGoogle Scholar
Gutenberg, B., and Richter, C. F., 1941. Seismicity of the Earth. Geol. Soc. Am., Sp. Paper no. 34, 131 pp.Google Scholar
Hess, H., 1938. Gravity Anomalies and Island Arc Structure with particular reference to the West Indies. Proc. Am. Phil. Soc., 79, 71–96.Google Scholar
Hess, H., 1948. Major Structural Features of the Western North Pacific, and interpretation of H. O. 5485, Bathymetric Chart, Korea to New Guinea. Bull. Geol. Soc. Am., 59, 417–446.CrossRefGoogle Scholar
Miller, B. J., 1937. Geophysical Investigations in the Emerged and Submerged Atlantic Coastal Plain–Pt. II, Geological Significance of the Geophysical Data. Bull. Geol. Soc. Am., 48, 803–812.CrossRefGoogle Scholar
Shepard, F. P. (1941), in Shepard, F. P. and Emery, K. O., 1941. Submarine Topography off the California Coast: Canyons and Tectonic Interpretations. Geol. Soc. Am., Sp. Paper No. 31, 109–159.Google Scholar
Shepard, F. P. 1948 a. Submarine Geology. Harper, 190–4.Google Scholar
Shepard, F. P. 1948 b. Evidence of World-Wide Submergence. Journ. of Marine Research, vii, 661–678.Google Scholar
Storm, L. W., 1945. Resumé of facts and opinions on sedimentation in the Gulf Coast region of Texas and Louisiana. Bull. Amer. Assoc. Petrol. Geol., 29, 1304–1335.Google Scholar
Umbgrove, J. H. F., 1947. The Pulse of the Earth, 2nd ed. The Hague, 97–143.CrossRefGoogle Scholar
Veatch, A. C., and Smith, P. A., 1939. Atlantic Submarine Valleys of the United States and the Congo Submarine Valley. Geol. Soc. Am., Sp. Paper No. 7, 33–7.Google Scholar
Willis, B., 1936. East African Plateaus and Rift Valleys. Carnegie inst. of Washington, Publ. No. 470, 358 pp.Google Scholar