between an abyssal plain and continental slope.
The area you are referring to is known as the continental rise. It is located at the base of the continental slope and consists of a thick accumulation of sediments that have been transported down from the continent. The continental rise marks the transition between the continental margin and the deep ocean basin.
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.
The continental shelf, continental slope, and continental rise combine to form the continental margin.
The continental shelf, continental slope, and continental rise combine to form the continental margin. The continental margin is the transition zone between the continent and the deep ocean basin.
The continental shelf, continental slope, and continental rise together form the continental margin. The continental margin is the submerged edge of a continent that consists of these three distinct but connected features.
downslope from the continental shelf
The area you are referring to is known as the continental rise. It is located at the base of the continental slope and consists of a thick accumulation of sediments that have been transported down from the continent. The continental rise marks the transition between the continental margin and the deep ocean basin.
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.
The continental shelf, continental slope, and continental rise combine to form the continental margin.
continental margin
The three parts of the continental margins are the Continental shelf, the Continental slope, and the Continental rise.
continental rise
The oceanic crust begins at the continental rise
The continental shelf, continental slope, and continental rise combine to form the continental margin. The continental margin is the transition zone between the continent and the deep ocean basin.
continental rise
The continental shelf, continental slope, and continental rise together form the continental margin. The continental margin is the submerged edge of a continent that consists of these three distinct but connected features.