continental slope
The average depth of the continental slope in the Atlantic Ocean is around 700 to 2,000 meters (2,300 to 6,560 feet). It can vary depending on the specific location and geological features in the region.
The three parts of the continental margins are the Continental shelf, the Continental slope, and the Continental rise.
The continental shelf, continental slope, and continental rise combine to form the continental margin.
Continental slope, Continental Rise, Continental Slope, Seamont, Trench
The continental shelf starts from the shore to a few miles out with less gradient of slope. The continental slope starts after shelf-break with a higher slope gradient, then follows the continental rise and abyssal-plain.
A sharp drop-off beyond the continental shelf is called a continental slope. The continental slope marks the transition between the continental shelf and the deep ocean floor.
A continental margin is NOT a part of a continent. It is the submerged outer edge of a continent that includes the continental shelf, continental slope, and continental rise.
continental margin
The continental shelf is a flattish area which extends from the shore out into the ocean and is made of continental crust. This ends in a slope (the continental slope) which descends to the abyssal plane, which is made of oceanic crust.
continental rise
Continental shelf.
Abrasion