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  • Volcanic Landforms at Divergent Plate Boundaries: Mid-Ocean Ridges Explained
    The volcanic landforms at divergent ocean plate boundaries are mid-ocean ridges. Here's why:

    * Divergent Plate Boundaries: These are areas where tectonic plates move apart.

    * Magma Upwelling: As plates pull away, it creates space for magma from the Earth's mantle to rise to the surface.

    * Volcanic Activity: This rising magma erupts, forming underwater volcanoes and volcanic islands.

    * Mid-Ocean Ridge Formation: Over time, these volcanic eruptions create a continuous chain of mountains under the ocean called a mid-ocean ridge.

    Key Features of Mid-Ocean Ridges:

    * Central Rift Valley: A depression in the middle of the ridge where new crust is forming.

    * Hydrothermal Vents: Hot springs that release chemicals and minerals from the Earth's interior.

    * Pillow Lavas: Unique lava formations that solidify in water.

    Examples:

    * Mid-Atlantic Ridge: The most well-known mid-ocean ridge, running down the center of the Atlantic Ocean.

    * East Pacific Rise: Another prominent mid-ocean ridge in the Pacific Ocean.

    Let me know if you'd like more information about these volcanic landforms!

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