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It is the largest known ocean canyon off the East Coast of the United States, and one of the largest submarine canyons in the world. The canyon is located near the 100 m (330 ft) isobath on the continental shelf and is 2.2 km (1.4 mi) deep at the base of the continental slope. Over an 80 km (50 mi) distance, the average slope of the canyon ...
The Cayman Trough (also known as the Cayman Trench, Bartlett Deep and Bartlett Trough) is a complex transform fault zone pull-apart basin which contains a small spreading ridge, the Mid-Cayman Rise, on the floor of the western Caribbean Sea between Jamaica and the Cayman Islands. [1]
The shelf usually ends at a point of increasing slope [3] (called the shelf break). The sea floor below the break is the continental slope. [4] Below the slope is the continental rise, which finally merges into the deep ocean floor, the abyssal plain. [5] The continental shelf and the slope are part of the continental margin. [6]
Cross section of an oceanic trench formed along an oceanic-oceanic convergent boundary The Peru–Chile Trench is located just left of the sharp line between the blue deep ocean (on the left) and the light blue continental shelf, along the west coast of South America.
The Ross Ice Shelf is the main outlet for several major glaciers draining the West Antarctic Ice Sheet, which contains the equivalent of 5 m of sea level rise in its above-sea-level ice." The report added that observations of "iceberg calving" on the Ross Ice Shelf are, in their opinion, unrelated to its stability. [10]
The continental shelf of the United States is one of the largest examples of marine geology in the world, with thousands of miles of submarine land making up the various shelves of the collective. Each different shelf features different extents of continental shelves, from the long, elevated shelves of Alaska , to the short shelf of the Pacific ...
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