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  • Mid-Ocean Ridges: Formation, Characteristics & Divergent Plate Boundaries
    Mid-ocean ridges are formed at divergent plate boundaries.

    Here's why:

    * Divergent boundaries are where tectonic plates move apart.

    * As the plates separate, magma from the Earth's mantle rises to the surface.

    * This magma cools and solidifies, creating new oceanic crust.

    * The process of new crust formation pushes the plates further apart, resulting in the formation of a mid-ocean ridge.

    Key Features of Mid-Ocean Ridges:

    * Underwater mountain range: Mid-ocean ridges are the longest mountain ranges on Earth, but they are submerged beneath the ocean.

    * Volcanic activity: They are characterized by active volcanism, as magma continuously rises to fill the gap between the separating plates.

    * Hydrothermal vents: These are areas where hot, mineral-rich water is released from the ocean floor, supporting unique ecosystems.

    * Earthquakes: The movement of the plates along divergent boundaries causes frequent earthquakes.

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