submarine canyons
V-shaped valleys in the continental shelf and slope are called submarine canyons. These are deep, steep-sided valleys that cut across the continental margin and are often formed by underwater processes such as turbidity currents or erosion by underwater currents. Submarine canyons can be comparable in scale to canyons found on land.
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.
The portion of the continental margin that serves as a boundary between the oceanic crust and the continental crust is called the continental shelf. This is the shallowest part of the margin, located between the shoreline and the continental slope.
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 continental shelf, continental slope, and continental rise combine to form the continental margin.
V-shaped valleys in the continental shelf and slope are called submarine canyons. These are deep, steep-sided valleys that cut across the continental margin and are often formed by underwater processes such as turbidity currents or erosion by underwater currents. Submarine canyons can be comparable in scale to canyons found on land.
Submarine Canyons
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.
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.
It is part of a continental plate that is submerged by the ocean. At the edge of the continental shelf, the slope suddenly increases and begins to drop off, this is called the continental slope.
They are both part of the larger structure called the continental margin where a continental plate meets an oceanic plate. The lower (deeper) end of the continental slope is called the continental rise.
continental slope
You can't have a continent rise from land, but you can have land rise from the continental shelf, which may be under water, and that is called an island.
The answer is: B. Continental slope.
The edge is called the shelf break. The actual declining shelf is called the called the continental slope.
Plateau, peak and slope. Valleys are the area between these forms.