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  • Volcanic Mountain Formation at Active Continental Margins: An Explanation
    At active continental margins, the primary type of mountain formation is volcanic mountain formation.

    Here's why:

    * Active margins are where an oceanic plate subducts beneath a continental plate.

    * Subduction causes the sinking plate to melt, generating magma.

    * This magma rises to the surface and erupts, forming volcanoes.

    * Over time, these volcanic eruptions can build up layers of lava and ash, creating volcanic mountains.

    Examples of volcanic mountains formed at active continental margins include:

    * The Andes Mountains in South America

    * The Cascade Range in North America

    * The Mount Fuji in Japan

    While folded mountains can also occur at active margins, their formation is more common at convergent plate boundaries where two continental plates collide.

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