The continental shelf, continental slope, and continental rise combine to form the continental margin.
continental margin
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 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.
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.
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, 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 continental shelf, slope, and rise combine to form the continental margin. The continental shelf is the shallow, submerged extension of a continent, the slope is the steep incline that leads to the ocean floor, and the rise is the gently sloping accumulation of sediment at the base of the slope. Together, they make up the transition zone between the continent and the deep ocean.
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.
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.
continental shelf
The continental shelf is basically an extension of a continent into an ocean. It is underwater during interglacial periods (such as today) but dry during glacial periods. The continental slope is the sloping area between the continental shelf and the continental rise (where the continental plate meets the oceanic plate). The continental shelf and the continental slope together are called the continental margin. The continental rise is located at the bottom of the continental slope and is formed by the accumulation of sediment from the continent. Past the continental rise lies the abyssal plain which is the flat ocean floor.