At mid-ocean ridges, tectonic plates diverge, allowing magma from the mantle to rise and create new oceanic crust as it solidifies. This process, known as seafloor spreading, results in the formation of underwater mountain ranges. Additionally, mid-ocean ridges are sites of significant geological activity, including volcanic eruptions and hydrothermal vent systems, which support unique ecosystems. Overall, they play a crucial role in the dynamic processes of plate tectonics and the Earth's geology.
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