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  • Understanding Convergent Plate Boundaries and Subduction Zones
    When one tectonic plate descends beneath another, it forms a convergent boundary.

    Specifically, this is a subduction zone. Here's why:

    * Convergent: The plates are moving towards each other.

    * Subduction: The denser plate (usually oceanic) sinks beneath the less dense plate (either oceanic or continental).

    This process leads to a variety of geological features, including:

    * Volcanoes: Magma rises from the melting plate, creating volcanoes.

    * Earthquakes: The friction and pressure along the boundary can cause earthquakes.

    * Mountain Ranges: The collision of the plates can push up mountains.

    * Trench: The area where the descending plate bends downwards forms a deep ocean trench.

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