continental slope. :)
The continental shelf, continental slop and the ocean floor
abyssal plain
The answer is: B. Continental slope.
The average width of the continental shelf is about 80 km or 50 miles. The Shelf descends steeply down to the continental rise before reaching the ocean floor.
the continental slope
The continental margin is the zone of ocean floor that separates oceanic crust and continental crust. It accounts for 28% of all oceanic area.
The continental shelf, continental slop and the ocean floor
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.
Continental shelf Continental slope abyss/abyssal plain
A continental margin is the zone of transition between a continent and the deep ocean floor. It includes the continental shelf, continental slope, and continental rise. It is an area where sediments from the continent are deposited and tectonic activity can occur.
Continental Shelf.
Continental shelf.
Continental shelf.
The ocean floor can be described in terms of three primary features: the continental shelf, continental slope, and continental margin. The continental shelf is the shallow, submerged extension of the land, where the ocean is relatively shallow and rich in marine life. Beyond the shelf, the continental slope descends steeply to the deep ocean floor, marking the transition from the shallow coastal waters to the deep sea. The continental margin encompasses both the shelf and slope, forming the boundary between the continental crust and the oceanic crust.
continental shelf
The deep, dark, ocean floor past the continental shelf, and the shallower, lighter, depths of the continental shelf.
The area between the continental shelf and the ocean floor is known as the continental slope. This region marks the transition from the relatively shallow waters of the continental shelf to the deeper oceanic depths. The continental slope is characterized by a steep gradient and is often where sediment from the shelf accumulates, leading to an important zone for marine life and geological processes.