Submarine Canyons
Submarine canyons. These are steep-sided valleys that cut into the continental slope and sometimes extend onto the continental shelf. Submarine canyons can be formed by various processes, including erosion from turbidity currents or underwater landslides.
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.
actually,the continental shelf is roughly 3,000,000 m. long
The part of a continent that is under water is called a continental shelf. It is the shallow submerged edge of a continent that extends from the shoreline to a steeper drop-off called 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.
shelf
Submarine Canyons
The edge is called the shelf break. The actual declining shelf is called the called the continental slope.
Submarine canyons. These are steep-sided valleys that cut into the continental slope and sometimes extend onto the continental shelf. Submarine canyons can be formed by various processes, including erosion from turbidity currents or underwater landslides.
It is called the continental shelf.
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 continental shelf layer is called the shelf break. It is the steepest part of the continental shelf where the seafloor drops off sharply towards the deeper 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.
The continental shelf, continental slop and the ocean floor
continental shelf peninsula
actually,the continental shelf is roughly 3,000,000 m. long
Continental Shelf