The continental shelf is the border of any of the continents that extends out and down to the ocean floor. It consists of slopes, rises and underwater canyons.
land -> continental shelf -> continental slope -> continental rise -> ocean floor.
The continental shelf, continental slope, and continental rise together form the continental margin. The continental margin is the submerged edge of a continent that consists of these three distinct but connected features.
shelf
The continental shelf, continental slope, and continental rise together form the continental margin. This is the outer edge of a continent where it transitions to the ocean basin. The continental margin is characterized by these three distinct topographical features.
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.
Some examples of continental shelves include the North American Continental Shelf, the Australian Continental Shelf, and the South American Continental Shelf. Each of these shelves extends from the continent's coast to varying distances into the ocean before dropping off into deeper waters.
Land. Continental shelf.
the continental shelf-edge or shelf-break
the oldest continental shelf is in tortoga
continental shelf
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.