Hostname: page-component-586b7cd67f-g8jcs Total loading time: 0 Render date: 2024-11-20T08:52:28.009Z Has data issue: false hasContentIssue false

Erosion of a Rock Floor by Tidal Sand Streams

Published online by Cambridge University Press:  01 May 2009

D. T. Donovan
Affiliation:
National Institute of Oceanography, Wormley, Surrey.
A. H. Stride
Affiliation:
Department of Geology, University of Bristol.

Abstract

Some closed basins extending along the strike of soft rocks in the English and Bristol Channels were cut by sand moved by tidal currents.

Type
Articles
Copyright
Copyright © Cambridge University Press 1961

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

Donovan, D. T., Savage, R. J. G., Stride, A. H., and Stubbs, A. R., 1961. Geology of the floor of the Bristol Channel. Nature, Lond., 189, 51–2.CrossRefGoogle Scholar
Donovan, D. T., and Stride, A. H. (in press). An acoustic survey of the sea floor south of Dorset and its geological interpretation. Phil. Trans.Google Scholar
Kuenen, Ph. H., 1950. Marine Geology, Wiley, New York.Google Scholar
Pringle, J., and George, T. N., 1948. South Wales. Brit. reg. Geol.Google Scholar
Sager, von G., 1961. Die Grösstgeschwindigkeiten der Gezeitenströrme zur mittleren Springzeit in der Nordsee, dem Kanal und der Irischen See. Beiträge zur Meereskunde, 1, 1926.Google Scholar
Stride, A. H., 1959. A pattern of sediment transport for sea floors around southern Britain. Dock. Harb. Author., 40, 145–7.Google Scholar
Stride, A. H., and Cartwright, D., 1958. Sand transport at southern end of the North Sea. Dock Harb. Author., 38, 323–4.Google Scholar