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.
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.
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.
The sharp drop from the continental shelf to the continental rise is called the continental slope. This transition zone marks the boundary between the relatively shallow waters of the continental shelf and the deeper ocean floor. The slope typically features steep gradients and can be characterized by various geological formations and sediment deposits.
Land. Continental shelf.
the continental shelf-edge or shelf-break
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.
the oldest continental shelf is in tortoga
continental shelf