The part on where the continental shelf meets the continental slope creating an edge.
A continental margin is NOT a part of a continent. It is the submerged outer edge of a continent that includes the continental shelf, continental slope, and continental rise.
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. 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.
actually,the continental shelf is roughly 3,000,000 m. long
A continental margin is NOT a part of a continent. It is the submerged outer edge of a continent that includes the continental shelf, continental slope, and continental rise.
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. 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.
actually,the continental shelf is roughly 3,000,000 m. long
shelf
The edge of a continental shelf is called the "shelf break." This is the point where the seabed steeply descends into the continental slope, marking the transition from the relatively shallow waters of the continental shelf to the deeper oceanic waters. The shelf break typically occurs at depths of around 100 to 200 meters, although this can vary depending on the geographical location.
Land. Continental shelf.
The continental margin is the submerged outer edge of a continent. It is generally divided into two sections: the continental shelf and the continental slope.
the continental shelf-edge or shelf-break
The area between the shoreline and the continental slope is known as the continental shelf. It is a relatively shallow, flat or gently sloping underwater landmass that extends from the shoreline to the beginning of the continental slope. The continental shelf is an important zone for marine life and for human activities such as fishing, oil and gas exploration, and shipping.
The continental shelf is the term for part of a continent that extends outward from the landmass beneath shallow seawater. The drop-off point of a continental shelf is called the shelf break. From this point, the continental goes down to the deep ocean floor.