You can get oil, coal, and patrolium. The patrolium can be used for JELLY! :D
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 continental shelf is the border of any of the continents that extends out and down to the ocean floor. It consists of slopes, rises and underwater canyons.
A continental shelf is an area where a country has some exclusive rights i e exploration of natural resources ,it can construct structures , it has also sovereignty over the water body.Other country only can cruse through without permission of concern country.It constitutes at the beginning of the sea up to the 350 km and it goes until the shelf drifts to deep bottom of sea.Hossain
All benthos live on the ocean floor, from the continental shelf to the abyssal plain. Some attach themselves to the floor, while others burrow under the sand. Continental shelf for A+.
North America And Europe
The continental slope is the area between the offshore shallows out to where the continental shelf dips steeply to the sea floor. It connects those two areas. The continental shelf is where the shallow waters of the ocean meet the shore. Farther out, the water gets progressively deeper, and this is the continental slope. At the outer edge of the continental slope, the bottom drops sharply away and plunges to the deep ocean. The Wikipedia article has more information and some drawings and diagrams. A link is provided. The steep slopingpart of the ocean floor termination of continental shelves is called continental slope.
There is an area of shallow water extending beyond the shoreline for some distance. At some point, the dropoff becomes very steep; this is the boundary of the continental shelf. For legal purposes, a depth of 600 feet is considered the edge of the shelf. On the eastern coast of North America, the shelf extends a great distance. Along the west coast, the shelf is almost non-existent; the water drops off to abyssal depths very close to shore.
It is the deepest, darkest area of the ocean beyond the edge of the continental shelf.
The continental shelf typically extends from the coastline to a depth of about 200 meters (656 feet) and can stretch for several hundred kilometers offshore, depending on the geographical area. Its width varies significantly around the world, with some shelves being quite narrow and others, like the Siberian shelf, extending up to 1,500 kilometers (932 miles) from the shore. Beyond the shelf, the ocean floor drops steeply into the continental slope and then into the deep ocean basin.
The rocks found in a continental shelf are often sedimentary rocks, such as sandstone, shale, and limestone. These rocks are formed from the accumulation of sediments on the ocean floor over long periods of time. Additionally, some continental shelves may also have igneous rocks brought up from volcanic activity.
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Some minerals being discovered in the continental shelf include manganese nodules, cobalt-rich ferromanganese crusts, polymetallic sulfides, and rare earth elements. These minerals have attracted interest due to their potential economic value and increasing demand in various industries.