Tectonic forces and the climate control the shape of the continental shelf. The continental shelf is the part of the continent that extends into the ocean.
The shape of the continental slope is primarily controlled by gravitational forces, erosion by currents and waves, and tectonic processes such as subsidence and uplift. These forces work together to shape the steep boundary between the continental shelf and the deep ocean floor.
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.
The widest continental shelf in Florida is the Gulf continental shelf. It is along the central-west coast of the state.
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.
Tectonic forces and the climate control the shape of the continental shelf. The continental shelf is the part of the continent that extends into the ocean.
The shape of the continental slope is primarily controlled by gravitational forces, erosion by currents and waves, and tectonic processes such as subsidence and uplift. These forces work together to shape the steep boundary between the continental shelf and the deep ocean floor.
shelf
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.
contiental shelf \
The widest continental shelf in Florida is the Gulf continental shelf. It is along the central-west coast of the state.
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.