Mid-ocean ridges form primarily due to tectonic plate movements at divergent boundaries, where two oceanic plates pull apart. As these plates separate, magma from the mantle rises to fill the gap, creating new oceanic crust. Additionally, the release of pressure and the presence of mantle plumes can contribute to volcanic activity along these ridges, further shaping the underwater landscape. This continuous process leads to the formation of long, underwater mountain ranges known as mid-ocean ridges.
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