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.
Geological exploration in an East Coast submarine canyon from a research submersible
Science
By: J. V. A. Trumbull and M.J. McCamis
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Abstract
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Geological exploration in an East Coast submarine canyon from a research submersible |
| Series title | Science |
| DOI | 10.1126/science.158.3799.370 |
| Volume | 158 |
| Issue | 3799 |
| Year Published | 1967 |
| Language | English |
| Publisher | AAAS |
| Description | 3 p. |
| First page | 370 |
| Last page | 372 |
| Google Analytic Metrics | Metrics page |