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These currents make up 90% of the ocean waters.These waters move around the ocean basins due to variations in the density and gravity.Deep waters sinks into the deep ocean basins at high latitudes , where the temperatures are cold enough to cause the density to increase.
The movement of deep water in the ocean basins is by density driven forces and gravity.
The ocean is deep because of the Earth's crust, which is thinner under the ocean than on land. This allows more space for water to fill, creating the deep ocean basins. Additionally, the movement of tectonic plates can also create deep trenches in the ocean floor.
To investigate the evolution of ocean basins by core drilling of ocean sediments and underlying oceanic crust.
turbidity currents, which are fast-moving underwater currents that carry sediment down into the deep ocean basins. These currents can transport large volumes of sediment over long distances before depositing them on the ocean floor.
The Intertidal zone, Coastal Ocean, and the Open Ocean
They are: Continental Shelf Continental Slope Abyssal Plain Ocean Deeps
The dust falls from the atmosphere over the ocean, sinks through the water column and ends up as sediments on the ocean floor.
The depth of an ocean basin varies significantly, but on average, ocean basins are about 12,080 feet (3,682 meters) deep. The Mariana Trench, the deepest part of the world's oceans, reaches approximately 36,000 feet (10,972 meters). Ocean basins can also include features like continental shelves and abyssal plains, leading to varied depths across different regions.
the continental Margin, Ocean Basin Floor and Mid-Ocean ridge :D
piles of basaltic lava flows built up from the ocean floor by multiple, summit and flank eruptions