submarine canyons
Submarine Canyons
Continental slope
Here is a pic of the continental slope.
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.
Between the continental slope and the ocean basin is the continental rise
Submarine Canyons
Submarine Canyons
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.
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.
The tip of the continental shelf (which has a gentle slope) where if you go any farther, the continental slope forms, which has a very steep slope.
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.
Continental slope
continental slope
The answer is: B. Continental slope.
The edge is called the shelf break. The actual declining shelf is called the called the continental slope.