Comparatively it has.
The continental shelf, continental slope, and continental rise combine to form the continental margin.
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.
A continental margin is NOT a part of a continent. It is the submerged outer edge of a continent that includes the continental shelf, continental slope, and continental rise.
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 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.
Yes, the continental shelf does have a slope, although it is generally very gentle. The slope leads down to the continental slope, which is a steeper gradient that marks the transition to the deep ocean floor. The continental shelf typically extends from the coastline to the shelf break, where the slope begins. Overall, the slope of the continental shelf is crucial for marine ecosystems and resource distribution.
The continental shelf, slope, and rise are all part of the continental margin. The continental shelf is the flat, shallow portion closest to the shore, followed by the continental slope, which descends steeply to the ocean floor. The continental rise is a gentle incline at the base of the continental slope. These features are connected and represent the transition from the continent to the deep ocean basin.
A passive continental rise is a gentle slope between the continental slope and the deep ocean floor. It is formed by sediments that accumulate from the erosional processes on the continental slope. The sediments typically consist of finer grains such as silt and clay.
A continental rise forms where the continental slope levels off, and sediment accumulates due to gravity transporting sediments downslope from the slope above. This is a gentle accumulation of sediments deposited by turbidity currents, rivers, and other geological processes at the base of the slope.
No, a continental slope is not gentle; it is characterized by a steep incline that connects the continental shelf to the deep ocean floor. Typically, the slope can range from a few degrees to over 25 degrees, making it much steeper than the surrounding areas. This steep gradient plays a crucial role in oceanic processes, including sediment transport and marine life habitats.
the slope.
The answer is that they are diffrent
Two different origins for the continental rise are turbidity currents depositing sediments at the base of the continental slope, forming a wedge-shaped accumulation, and sediment transported by rivers accumulating at the continental margin, leading to the gradual build-up of a gentle slope.
You can't have a continent rise from land, but you can have land rise from the continental shelf, which may be under water, and that is called an island.
continental slope
The Slope
slope