The Entire Ocean Floor Is Covered By Sediments

This is enough to cover the entire ocean floor with 97 500 feet 18 5 miles of sediment.

The entire ocean floor is covered by sediments. Some may call this sediment biogenous sediment and this sediment roughly covered 75 of deep seafloor and one of the most important constituents of ocean sediments. An is the vast relatively deep flat sediment covered portion of the deep ocean basin. The features of the ocean floor are covered by a layer of sediments the thickness of which depends on the age of the feature the local topography and on the abundance of the sediment sup ply. The ocean basin floor is everywhere covered by sediments of different types and origins.

For many years scientists have studied the ocean s creatures the effects of introducing chemicals to the water and the geologic floor of the world s vast oceans. The fact that most of the earth is covered in water has spurred much interest in the world s oceans. Calcareous oozes and siliceous oozes. Terrigenous sediment is the most abundant sediment found on the seafloor followed by biogenous sediment.

The only exception are the crests of the spreading centres where new ocean floor has not existed long enough to accumulate a sediment cover. The sediments that accumulate there come from a variety of sources. Ocean basin ocean basin deep sea sediments. Ocean floor sediments sediment on the seafloor originates from a variety of sources including biota from the overlying ocean water eroded material from land transported to the ocean by rivers or wind ash from volcanoes and chemical precipitates derived directly from sea water.

Submarine sediments are of two main types. Calcareous oozes are. The sediment in areas of the ocean floor which is at least 30 biogenous materials is labeled as an ooze. The only exception are the crests of the spreading centres where new ocean floor has not existed long enough to accumulate a sediment cover.

The ocean floor is a sort of ultimate collection pan for the entire globe. Abyssal plain a marks the site where old oceanic lithosphere begins its descent into a subduction zone. Plankton is the contributor of oozes. There are two types of oozes.

Sediment thickness in the oceans averages about 450 metres 1 500 feet. In order to produce this colossal quantity of sediment an incredible layer of rock 200 000 feet 38 miles thick would have to be eroded off of the continents. The ocean basin floor is everywhere covered by sediments of different types and origins. This sediment is composed of clay particles and microskeletons of oceanic organisms that sink slowly through the water column to the ocean floor.