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  • Understanding Pull-Apart Rift Zones: Divergent Plate Boundaries
    The plate boundary associated with a pull-apart rift zone is a divergent boundary.

    Here's why:

    * Divergent boundaries are where tectonic plates move apart. This separation causes the lithosphere (Earth's crust and upper mantle) to thin and break.

    * Rift zones are areas where the Earth's crust is being pulled apart, leading to the formation of valleys, volcanoes, and earthquakes.

    * Pull-apart rift zones are a specific type of rift zone where the plates are moving horizontally apart, creating a "pull-apart" effect. This can lead to the formation of grabens (down-dropped blocks of crust) and other geological features.

    Examples:

    * The East African Rift Valley is a classic example of a pull-apart rift zone where the African plate is splitting.

    * The Mid-Atlantic Ridge is another example of a divergent boundary where new oceanic crust is being formed as the plates pull apart.

    Therefore, pull-apart rift zones are a direct consequence of the divergent plate boundary process.

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