Geology and biology of Oceanographer submarine canyon.

Marine Geology
By: , and 



Santonian beds more than 100 m thick are the oldest rocks collected from the canyon. Quaternary silty clay veneers the canyon walls in many places and is commonly burrowed by benthic organisms that cause extensive erosion of the canyon walls, especially in the depth zone (100-1300 m) inhabited by the crabs Geryon and Cancer. Bioerosion is minimal on high, near-vertical cliffs of sedimentary rock, in areas of continual sediment movement, and where the sea floor is paved by gravel. A thin layer of rippled, unconsolidated silt and sand is commonly present on the canyon walls and in the axis. Shelf sediments are transported from Georges Bank over the E rim and in the Canyon by the SW drift and storm currents; tidal currents and internal waves move the sediment downcanyon along the walls and axis.- from Authors
Publication type Article
Publication Subtype Journal Article
Title Geology and biology of Oceanographer submarine canyon.
Series title Marine Geology
DOI 10.1016/0025-3227(80)90004-3
Volume 38
Issue 4
Year Published 1980
Language English
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Marine Geology
First page 283
Last page 312
Google Analytic Metrics Metrics page
Additional publication details