* Volcanic arcs: Chains of volcanoes that form on the overriding plate, often parallel to the trench. These volcanoes erupt with magma generated by the melting of the subducting plate.
* Deep-sea trenches: These are the deepest parts of the ocean floor, formed where the descending plate bends downwards.
* Fold mountains: As the plates collide, the overriding plate can be folded and uplifted to form mountain ranges.
* Earthquakes: Subduction zones are some of the most active earthquake zones on Earth, as the plates grind past each other.
Examples of subduction zones and the landforms they produce include:
* The Andes Mountains: These mountains are a result of the Nazca Plate subducting beneath the South American Plate.
* The Mariana Trench: The deepest point on Earth, formed by the Pacific Plate subducting beneath the Philippine Plate.
* The Aleutian Islands: A volcanic arc formed by the Pacific Plate subducting beneath the North American Plate.
So, the type of landforms that develop at these plate boundaries are a combination of volcanic arcs, deep-sea trenches, fold mountains, and active earthquake zones.
