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What is Continental Slope definition/concept

Below the depths of the sea are the so-called submerged reliefs. These reliefs are found both at the bottom of the seas and in the oceans. Continental Slope

Depending on its geological origin, there are two types of relief:

1) reliefs that lie on the continental margin and are located below the earth’s crust;

2) the reliefs of the ocean floor, which are characteristic of the oceanic crust.

Within the reliefs of the continental margin there is the platform Continental, which is the extension of certain areas of land and have a gentle slope that goes from the coast to about 200 meters deep. In coastal areas, the corresponding continental shelves are generally gentle slopes, whereas in mountainous areas close to the coast of the  continental shelf they are usually much more pronounced. Continental Slope

The continental slope is next to the continental shelf

The area has a steep slope type and in terms of location it is between the end of the continental shelf and the foot of the slope, where it comes into contact with the ocean floor.

The slope goes from 200 meters deep in its upper part to 3500 meters deep in its lower part. The foot of the slope is formed by the accumulation of sediments fallen from the s a steep slope type and in terms of location it is between the end of the continental shelf. Anyway, it forms a part of the underwater morphology. In this type of relief , valleys, mountains and large underwater canyons appear.

Due to its great depth, the continental slopes do not receive sunlight and the water temperature is very low. In this extreme environment we can find giant craters that emit gases such as methane hydrate. On oceanic slopes this gas remains stable, but if the temperature changed this gas would escape from the depth of the aquatic environment and cause damage to the environment, or else serious accidents with the vessels. Continental Slope

Other oceanic reliefs

In addition to the continental slopes, in the depths of the sea and oceans there are other types of relief. Thus, the abyssal plains are flat surfaces of great extensions and are covered with sediments. Some abyssal plains have breaks in the terrain, better known by the name of guyots (guyots are seamounts that have a conical shape and a flat top).

On the other hand, some abyssal plains are also interrupted by the so-called oceanic ridges, which are marine mountain ranges that extend along the oceans.

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