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  • Mid-Ocean Ridges: Formation, Composition & Seafloor Spreading
    The place where magma pushes up on oceanic lithosphere is called a mid-ocean ridge.

    Here's why:

    * Oceanic Lithosphere: This is the Earth's crust and upper mantle that exists beneath the ocean. It's relatively thin and dense.

    * Magma: Molten rock beneath the Earth's surface.

    * Mid-Ocean Ridges: These are underwater mountain ranges that run along the middle of the ocean basins. They are formed by the process of seafloor spreading.

    How it Works:

    1. Convection Currents: Deep within the Earth's mantle, convection currents (like giant boiling pots) bring hot magma towards the surface.

    2. Divergent Plate Boundaries: At mid-ocean ridges, tectonic plates are moving apart (diverging).

    3. Upwelling Magma: As the plates separate, the pressure decreases, allowing the magma to rise and erupt.

    4. New Crust Formation: The erupted magma cools and solidifies, forming new oceanic crust. This process pushes the existing crust further away from the ridge, creating the spreading phenomenon.

    So, in essence, mid-ocean ridges are the locations where the Earth's internal heat drives the creation of new ocean floor through the process of magma pushing up on the oceanic lithosphere.

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