the continental Margin, Ocean Basin Floor and Mid-Ocean ridge :D
The continental margin is the zone of the ocean floor that separates the thin oceanic crust from thick continental crust.
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 Margin, Ocean Basin Floor and Mid-Ocean ridge :D
the continental Margin, Ocean Basin Floor and Mid-Ocean ridge :D
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.
The abyssal zone is not included in the continental margin. It is the deep ocean floor beyond the continental shelf, slope, and rise.
continental margin deep-ocean basin
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 relationship between the existence of the plume influence and ocean floor topography.
The ocean floor is divided into two major regions: the continental margin, which includes the continental shelf, slope, and rise, and the deep ocean basin, which includes abyssal plains, seamounts, trenches, and mid-ocean ridges. These regions have distinct geological features and play important roles in shaping the Earth's surface.
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.