What is a continental rise?

Continental rise is an underwater feature that is located between the continental slope and abyss. This function can be found worldwide and represents the final phase of the boundary between continents and the deepest part of the ocean. The environment in the continental rise is unique and many oceanographers study it extensively in the hope of learning more about the ocean and geological history.

before immersed in the specifics of a continental rise, it may have a quick overview of the main features of the ocean DNA, starting with a continental boss, with an open ocean and open ocean and open ocean and open ocean and open ocean Open awards, and on the continent, and open ocean and on the continent and open ocean, and on the open ocean and open ocean and on the continent and open municipalities and open awards. At some depth, the continental shelf begins to decrease sharply and creates a function called continentalslope. Unlike the continental shelf, the continental slope is somewhat steep, and geologists suspect that it can mean earlier levels of the sea of ​​the earth. In addition to the continental rise, the abysmal plane stretches, an extremely flat seabed area, which is also incredibly deep. To make the plain hosts many unique forms of life that are uniquely adapted to survival in its cold, high pressure and dark conditions. The equality of the abyss is interrupted by massive underwater mountain chains near the tectonic boundaries of the earth's plates.

The formation of a continental rise is a constant and very slow process. When rivers and streams travel on the ground, they pick up the sediment, mud and the assortment of another material that is gradually carried out to the sea. Some of these sediments settle on a continental shelf, but others carry a continental slope to create a continentvzestup. ContinentalThe rise is often very rich in nutrients, because of the sediments it contains, and can attract an assortment of underwater creatures looking for snacks.

These sea creatures contribute more sediments. Over the past millennium, the continental rise has become the shape of a thick wedge of the material that has settled at the bottom of the continental slope, similar to detritus, which accumulates on the base of the cliff. The function is named because it creates a characteristic sudden rise in ocean bottom, which is very distinctive on radar screens used by ships. It draws attention to the fact that it is approaching a continental shelf, suggesting that the soil cannot be too far away.