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The least amount of sediment accumulation will be at Spreading centers.

What are Spreading centers?

Deep cracks in the crust are created by spreading centers, which happen where two plates are drifting apart. By stretching the crust, magma from the upper mantle can rise to the surface and cool, generating basalt, which is a frequent volcanic rock. The Mid-Atlantic Ridge is a magnificent illustration.

Geologic zones are separated by spreading centers. At the center of the axis is the neovolcanic zone. It is between one and two kilometers broad and is the location of both hydrothermal vents and recent and active volcanism. Small volcano chains or volcanic ridges serve as its indicators. A seafloor region characterized by fissures is next to the neovolcanic zone. It could be between one and two kilometers wide.

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