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- W2017019301 abstract "Among the many speculations concerning the origin of submarine canyons, bottom-currents of various types have been appealed to frequently. This is one theory to which it is possible to apply some quantitative data, and to form an estimate as to the importance which may be attached to this means of producing submarine canyons, both now and in past ages. I refer of course to normal currents due to differences in densities caused by temperature and salinity, and to those which have a tidal origin, and not to the type recently proposed by Daly. Consequently during the summer of 1936 measurements of the bottom-currents were made in three of the submarine canyons of Georges Bank from the research vessel Atlantis of the Woods Hole Oceanographic Institution. Because of the physical difficulties of obtaining readings on the bottom in deep water, in a region where tidal currents at the surface are strong, the results are far from giving a complete picture. Nevertheless, some idea may be obtained of the magnitude of the velocities which might be expected." @default.
- W2017019301 created "2016-06-24" @default.
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- W2017019301 date "1937-01-01" @default.
- W2017019301 modified "2023-09-27" @default.
- W2017019301 title "Current-measurements in the Georges Bank Canyons" @default.
- W2017019301 doi "https://doi.org/10.1029/tr018i001p00216" @default.
- W2017019301 hasPublicationYear "1937" @default.
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