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terrigenous sediment
Sediment is a noun.
Sediments is the plural of sediment
they are deposited by sediment
Sediment
Convergence supports the theory of seafloor spreading. Samples of the deep ocean floor are evidence of seafloor spreading because the basaltic oceanic crust and overlapping sediment become younger as the mid-ocean ridge is approached. Also, the rock that makes up the floor of the ocean is younger than the continents.
Age of seafloor rock and sediment increases with distance from the oceanic ridges.
Convergence supports the theory of seafloor spreading. Samples of the deep ocean floor are evidence of seafloor spreading because the basaltic oceanic crust and overlapping sediment become younger as the mid-ocean ridge is approached. Also, the rock that makes up the floor of the ocean is younger than the continents.
terrigenous sediment
grab sampler
continental slope
Lowering the pH to less alkaline and more acidic levels would cause more calcareous materials to dissolve in seawater thereby reducing the abundance of calcareous sediment on the seafloor.
Near the trenches, or in the seafloor furthest away from spreading centers.
sediment cores
the thickest accumulation of sediment on the ocean floor is at the CONTINENTAL SLOPES AND RISES. :)
Marine sediments are typically terrigenous in nature, which means they came from the land. Sediments that originate from the continents are called terrigenous.
The trenches catch most of the sediment from the plates that break up and sink deeper into the water. This causes the upper plates to grow.