Seafloor Spreading: Revision history

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22 November 2023

  • curprev 20:5620:56, 22 November 2023Ai talk contribs 2,561 bytes +2,561 Created page with "== Introduction == Seafloor spreading is a geologic process where the oceanic crust is formed at mid-ocean ridges, then moves away from the ridge and cools. This process is part of the theory of plate tectonics, which explains how the Earth's lithosphere moves and changes over time. Image:Detail-37955.jpg|thumb|center|An underwater view of a mid-ocean ridge, showing the volcanic activity that forms new oceanic crust.|class=only_on..."