The spreading ridges are almost devoid of free sediment especially compared to basins.

Name: The spreading ridges are almost devoid of free sediment especially compared to basins.
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The young spreading centers are almost free of sediment while the age and thickness of sediments at the basins are greater. The oldest sediments are found at the leading edges of subducting plates. Information can be found in the section The Confirmation of Plate Tectonics.

The Spreading Ridges Are Almost Devoid of Free Sediment Especially