continental slopes
The continental shelf layer is called the shelf break. It is the steepest part of the continental shelf where the seafloor drops off sharply towards the deeper ocean floor.
A narrow shelf is often called a "slim shelf" or a "slender shelf".
continental slope, where the sea floor steeply drops off to deeper ocean depths. It marks the transition from shallow continental waters to the deeper oceanic realm.
Continental shelves typically end where the seafloor drops off into the open ocean, known as the continental slope. This transition point can vary in depth but is usually around 200 meters (656 feet) deep. Beyond the continental slope lies the deep ocean floor known as the abyssal plain.
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 continental shelf layer is called the shelf break. It is the steepest part of the continental shelf where the seafloor drops off sharply towards the deeper ocean floor.
The continental shelf
The steep side of the edge of a continent is called a continental slope. This feature marks the transition between the continental shelf and the deep ocean floor.
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.
the continental slope
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.
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 geologic edge of a continent is typically defined by the continental shelf, which is the submerged part of the continent that slopes downward into the ocean basin. This transition from the continental shelf to the deep ocean is called the continental slope.
A narrow shelf is often called a "slim shelf" or a "slender shelf".
continental slope, where the sea floor steeply drops off to deeper ocean depths. It marks the transition from shallow continental waters to the deeper oceanic realm.
The continental shelf, continental slope, and continental rise combine to form the continental margin. The continental margin is the transition zone between the continent and the deep ocean basin.
The edge is called the shelf break. The actual declining shelf is called the called the continental slope.