there is really no depth because continental rise is only little pieces of sediment.
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.
The continental shelf, continental slope, and continental rise combine to form the continental margin, which is the submerged outer edge of a continent that extends from the shoreline to the deep ocean floor.
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 slope is the steep transitional area between the shelf and rise. The continental slope depth for the Atlantic Ocean is 3900 meters or in other words 12800 feet.
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
continental rise
downslope from the continental shelf
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.
The Continental rise is often hundreds of kiometres. But in the pacific ocean it has a greater number.
Great White and tiger sharks live in the continental rise.