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USGS · 70011548

Geological exploration in an East Coast submarine canyon from a research submersible

J. V. A. Trumbull·M.J. McCamis
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Abstract

Large talus blocks litter the flat floor of Oceanographer Canyon at a depth of 1460 meters; they indicate down-axis mass transport of floor sediment at an unknown time and rate. From 1460 to 1310 meters the sidewall is covered by unconsolidated sediment lying at 35° to 40° from the horizontal. An outcrop of Pleistocene or younger sediment at 1460 meters is probably a remnant of a former fill.

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J. V. A. Trumbull, M.J. McCamis. 1967. Geological exploration in an East Coast submarine canyon from a research submersible. https://doi.org/10.1126/science.158.3799.370

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