continental trench
The subdivisions of the continenetal mmarging is the continental Slope, Continental Shelf and the Continental Rise
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.
land -> continental shelf -> continental slope -> continental rise -> 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.
Continental shelf is an undersea extension of a continent. Continental slope connects the continental shelf to the abyssal plain.
continental margin
The three parts of the continental margins are the Continental shelf, the Continental slope, and the Continental rise.
Same area: Lower part is continental shelf whereas the upper part is exclusive economic zone. Seabed or Subsoil is covered in continental shelf whereas above that is exclusive economic zone.
The subdivisions of the continenetal mmarging is the continental Slope, Continental Shelf and the Continental Rise
The three parts of the continental margins are the Continental shelf, the Continental slope, and the Continental rise.
The continental shelf starts from the shore to a few miles out with less gradient of slope. The continental slope starts after shelf-break with a higher slope gradient, then follows the continental rise and abyssal-plain.
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.
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.
continental margin
land -> continental shelf -> continental slope -> continental rise -> ocean floor.
Continental shelf, continental slope, continental rise and abyssal plain. The first three make up the continental margin.
The continental margin is the submerged outer edge of a continent. It is generally divided into two sections: the continental shelf and the continental slope.