Between the continental slope and the ocean basin is the continental rise
continental rises
The steep area between the continental shelf and the ocean floor is called the continental margin. A continental margin is usually composed of a steep continental slope that is followed by the flatter continental rise.
The zone of ocean under shelf and continental slope are continental.
20,000 to 30,000 thousand miles
The continental shelf is basically an extension of a continent into an ocean. It is underwater during interglacial periods (such as today) but dry during glacial periods. The continental slope is the sloping area between the continental shelf and the continental rise (where the continental plate meets the oceanic plate). The continental shelf and the continental slope together are called the continental margin. The continental rise is located at the bottom of the continental slope and is formed by the accumulation of sediment from the continent. Past the continental rise lies the abyssal plain which is the flat ocean floor.
continental rises
the answer to the question is: continental slope
the continental slope
continental slope
A sharp drop from a continent to an ocean basin is called a continental slope. This feature marks the boundary between the continental shelf and the deep ocean floor.
The best way to describe such a region would be as a continental slope. This area marks the boundary between the shallow continental shelf and the deep ocean floor. It is characterized by a steep incline leading down to the ocean basin.
The continental shelf, slope, and rise are all part of the continental margin. The continental shelf is the flat, shallow portion closest to the shore, followed by the continental slope, which descends steeply to the ocean floor. The continental rise is a gentle incline at the base of the continental slope. These features are connected and represent the transition from the continent to the deep ocean basin.
The Underwater landforms are the continentalshelf ,continental slope , continental rise , sea mounts , mid-ocean ridge ,abyssal plain , trench , and basin.
Submarine Canyons
Submarine Canyons
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 slope, Continental Rise, Continental Slope, Seamont, Trench