The Mid-Atlantic Ridge is a continuous mountain range that runs down the center of the Atlantic Ocean, formed by the tectonic activity of diverging oceanic plates. This underwater ridge is where new oceanic crust is created as magma rises from below the Earth's surface, leading to significant geological activity, including volcanic eruptions and earthquakes. It is also closely linked to geomagnetic reversals and magnetic anomalies, which provide vital information about Earth's geological history.
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