The continental shelf is a flattish area which extends from the shore out into the ocean and is made of continental crust. This ends in a slope (the continental slope) which descends to the abyssal plane, which is made of oceanic crust.
A sharp drop-off beyond the continental shelf is called a continental slope. The continental slope marks the transition between the continental shelf and the deep ocean floor.
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.
Yes, the continental slope is the relatively steep slope that connects the continental shelf to the deep ocean floor. It marks the boundary between the continental crust and oceanic crust.
The continental rise is between the continental shelf and the abyssal plain.LittoralLitoral (alternative spelling)Intertidal
The area between the shoreline and the continental slope is known as the continental shelf. It is a relatively shallow, flat or gently sloping underwater landmass that extends from the shoreline to the beginning of the continental slope. The continental shelf is an important zone for marine life and for human activities such as fishing, oil and gas exploration, and shipping.
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, 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 slope
The seaward edge of the continental shelf is marked by the shelf break, which is the steep slope that descends from the continental shelf to the deep ocean floor. This is where the ocean depth abruptly increases, indicating the boundary between the continental shelf and the continental slope.
The continental margin consists of three main subdivisions: the continental shelf, the continental slope, and the continental rise. The continental shelf is the shallow, gently sloping portion closest to the shore. The continental slope is the steeper portion that connects the shelf to the deep ocean floor. The continental rise is the transition zone between the slope and the deep ocean basin, where sediments accumulate.
The continental shelf, continental slope, and continental rise combine to form the continental margin.
The slope is the steep incline at the edge of the continental shelf that descends into the ocean depths. The continental shelf is a gently sloping, submerged portion of a continent that extends from the shoreline to the shelf break where the slope begins.