Oil and Coal
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 flattest part of the continental margin is typically found on the continental shelf, which is a gently sloping submerged platform that extends from the shoreline to the beginning of the continental slope. This region is characterized by relatively shallow waters and is an important area for marine life and coastal processes.
Some examples of continental shelves include the North American Continental Shelf, the Australian Continental Shelf, and the South American Continental Shelf. Each of these shelves extends from the continent's coast to varying distances into the ocean before dropping off into deeper waters.
The states in India with the broadest continental shelf are Gujarat, Maharashtra, and Kerala. These states have a wider continental shelf due to their geographical location along the western coast of India.
Yes, minerals can be found in the continental shelf. The continental shelf is an area of shallow water near the coastline where sediment and minerals can accumulate. These minerals can include sand, gravel, and even valuable resources like oil and gas.
The answer is TRUE
Mineral resources that can be harvested from the continental shelf include oil, natural gas, sand and gravel, phosphorite, and metallic minerals like manganese and iron. Seafloor mining operations are also being developed to extract rare earth elements and precious metals from certain areas of the continental shelf.
shelf
Land. Continental shelf.
the continental shelf-edge or shelf-break
The continental shelf starts from the shore to a few miles out with less gradient of slope. The continental slope starts after shelf-break with a higher slope gradient, then follows the continental rise and abyssal-plain.
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.
The widest continental shelf in Florida is the Gulf continental shelf. It is along the central-west coast of the state.