here you have it the answer is simply nothing it was here before humans before dinosaurs even so the answer is neither study hard and study here this is 101 percent true!
continental slope. :)
continental shelf
The continental rise.
The answer is: B. Continental slope.
the continental slope
Alluvial fans primarily involve constructive forces. They are formed when sediment-laden water flows down a slope and deposits sediments at the base, creating a fan-shaped landform. This process adds material to the landscape, thereby contributing to its construction and development. While erosion can occur in the surrounding areas, the formation of alluvial fans themselves is a constructive geological process.
continental slope
The three parts of the continental margins are the Continental shelf, the Continental slope, and the Continental rise.
Glaciers can be both constructive and destructive. They are constructive because they shape the landscape by eroding and transporting rocks and sediments, creating features like valleys and fjords. However, glaciers can also be destructive as they can erode bedrock and cause erosion, leading to changes in the landscape and potential hazards such as glacial outburst floods.
The continental shelf, continental slope, and continental rise combine to form the continental margin.
Continental slope, Continental Rise, Continental Slope, Seamont, Trench
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 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.
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.
continental margin
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.