A continental shelf is the continent feature that is submerged under an area of relatively shallow water this is known as the shelf sea. The shelves are greatly exposed by the drops in the sea level during the glacial periods. The shelf which is being surrounded by an island is known as the insular shelf.
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The margin which is located along the continent is situated between the continental shelf and the abyssal plain comprises a steep shaped continental slope which is surrounded by the continental rise, here the sediment from the continent which is above the cascades and down the slope has accumulated a pile of sediment which is at the base of the slope. This extends as far as 500 km (that is 310 mi) from the slope, this consists of the thick sediments which are deposited by the turbidity currents that are originated from the shelf and slope.
Continental shelf or the zone is a broad type, relatively shallow submarine terrace which is made up of continental crust this is formed at the edge of a continental landmass. The geological feature of the continental shelves is very much similar to that of the exposed portion of the continent which is located adjacent to it. Most of the shelves have a gentle rolling topographic feature which is called a ridge. The Continental shelves consist of about 8 percent of the entire area which is covered by oceanic landforms.
Structure of Continental Zone
A continental shelf extends from the coastal area to the depths of around 100–200 meters (that is approximately 330–660 feet). They are gently inclined towards the sea at an average slope of approximately 0.1°. In all such instances, the shelf ends towards the sea’s edge with an abrupt drop which is called the shelf break. Below here lies the continental slope which has a steeper zone that merges with the oceanic floor and this is called the continental rise. Here the depth is roughly 4,000 to 5,000 meters (which is moreover 13,000 to 16,500 calculated in feet).
Few continental margins like that of the Mediterranean coast of France and at the Porcupine Bank, off the western coast of Ireland, do not have a sharp definition of the slope but rather they maintain a generally convex shape structure towards the seafloor.
Widest Continental Shelf
The widest continental shelf on the planet extends to about 1,210 km (in miles it is 750 miles) it is located off the coast of Siberia, Russia, and into the Arctic Ocean. The Continental shelves serve as an extension of the coastal plains. They are marked by the wide-sloping submerged plains which are approximately 7.4% of the world's oceanic surface that sits above the continental shelves; they have a global average width of approximately 78 km (that is 48 miles).
The average width of the continental shelf is 65 km (that is 40 miles). Most of the continental shelves are very broad, gently sloping plains which are covered by relatively shallow type water. The water depth which is over the continental shelves is the average that are about 60 meters (which is 200 feet).
Continental Shelf Depth
A Continental Shelf Depth is about 60 meters. The average width of the continental shelf is around 65 km (that is 40 miles). Most of the continental shelves are very broad and are the gently sloping plains that are covered by relatively shallow water. The water depth is up to 60 meters (200 feet).
200 meters deep is the Continental Shelf of Australia.
This shelf is very shallow, which is up to 200 meters deep, much compared to the thousands of meters deep in the ocean, it extends outward to the continental slope which is quite deeper where the ocean begins.
100m is the continental margin. This is in the Atlantic Ocean, where the continental margins have a shelf that is broad and flat. This reaches a depth of 100 m. Here the slope is the steep transitional area that is between the shelf and the rise, and this lies between the depths of 100 and 2,500 m.
In geological meaning, a continental platform is an area that is covered by relatively flat or by gently tilted sedimentary strata. This is an overlie basement that has consolidated igneous or metamorphic rocks which are formed by an earlier deformation. The Platforms, the shield, and the basement rock together make up the cratons.
The Shelf seas or the continental sea refers to the ocean waters which are located on the continental shelf. Their wave motion is controlled by the summation influence of the tides, wind-forcing, and the brackish water which are formed from the river inflows. The regions are biologically highly productive, this is due to the mixing which is caused by the shallower waters and the enhanced current speeds. Despite all covering, only about 8% of the Earth's ocean surface area, that is the shelf seas supports 15-20% of global primary productivity.
Continental Shelf Location
The Continental Shelf is located at the edge of a continent that lies under an ocean. Here the continents are the main divisions of the land on this Earth. The continental shelf which extends from the coastline of a continent to a drop-off point is called the shelf break. From this break, the shelf descends to the deep ocean floor which is called the continental slope.
Continental Plain or the continental margin landform is the broad and gentle pitch of the continental shelf that gives way to the steeper continental slope. Gradual the transition more is the abyssal plain. Here the region is sediment-filled and is called the continental rise. The continental shelf, slope, and rise are collectively known as the continental margin.