downslope from the continental shelf
between an abyssal plain and continental slope.
The accumulation of sediment at the bottom of a continental slope is referred to as continental rise. This phenomenon occurs in oceans throughout the world.
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.
how much light does the continental rise
no.
continental margin
The three parts of the continental margins are the Continental shelf, the Continental slope, and the Continental rise.
The oceanic crust begins at the continental rise
continental rise
continental rise
They have a continental rise
Subduction. A subduction trench.