The area between the shoreline and the continental slope is the continental shelf.
The submerged land at the edge of a continent is called the continental shelf. It is an underwater landmass that extends from the shoreline to the continental slope.
An underwater plain that borders a continent is called a continental shelf. It is a relatively shallow area of the ocean that extends from the shoreline to the continental slope.
The true edges of continents are known as continental margins, which consist of the continental shelf, continental slope, and continental rise. These margins mark the transition from the continent to the ocean basin and can extend hundreds of kilometers from the shoreline.
The transition zone between an ocean basin floor and a continent is known as the continental shelf. It is the submerged part of a continent that extends from the shoreline to the continental slope. The continental shelf is characterized by relatively shallow waters and is an area of high biological productivity.
A sharp drop from a continent to an ocean basin is called a continental slope. This feature marks the boundary between the continental shelf and the deep ocean floor.
At the shoreline
The portion of the continental margin that serves as a boundary between the oceanic crust and the continental crust is called the continental shelf. This is the shallowest part of the margin, located between the shoreline and the continental slope.
contiental shelf \
The continental shelf, continental slope, and continental rise combine to form the continental margin, which is the submerged outer edge of a continent that extends from the shoreline to the deep ocean floor.
Deep sea trenches, Mountain ranges, Volcanoes, and Earthquakes.
The continental shelf, continental slope, and continental rise combine to form the continental margin. The continental margin is the outer edge of a continent that includes these three regions and extends from the shoreline to the deep ocean floor.
The seaward edge of the continental shelf is marked by the shelf break, which is the steep slope that descends from the continental shelf to the deep ocean floor. This is where the ocean depth abruptly increases, indicating the boundary between the continental shelf and the continental slope.
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.
It is called The Continental Shelf.
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The submerged land at the edge of a continent is called the continental shelf. It is an underwater landmass that extends from the shoreline to the continental slope.
The continental slope is the area of the ocean floor in which gently drops and is connected to the oceanic crust and continental shelf. This slope is caused by waves within the ocean.