mountains or volcanoes will appear
Yes, the continental slope descends steeply from the continental shelf into the deep ocean floor. It marks the boundary between the continental crust and the oceanic crust.
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.
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continental slope, where the sea floor steeply drops off to deeper ocean depths. It marks the transition from shallow continental waters to the deeper oceanic realm.
Yes, the continental slope is the relatively steep slope that connects the continental shelf to the deep ocean floor. It marks the boundary between the continental crust and oceanic crust.
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 process by which new material is added to the ocean floor along the boundary between diverging plates.
An ocean to continent boundary is where the oceanic crust meets the continental crust. This typically occurs at a continental shelf, which is the gently sloping transition between the continent and the ocean floor. This boundary is marked by significant differences in physical and geological characteristics between the two crust types.
The depth of the continental rise typically ranges from 3,300 to 13,200 feet (1,000 to 4,000 meters). It marks the boundary between the continental slope and the deep ocean floor, where sediment from the continent accumulates.
it subducts underneath the crustal plate
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 shape of the continental slope is primarily controlled by gravitational forces, erosion by currents and waves, and tectonic processes such as subsidence and uplift. These forces work together to shape the steep boundary between the continental shelf and the deep ocean floor.