Here's why:
* Subduction Zones: These are areas where one tectonic plate (the denser oceanic plate) slides beneath another (the continental plate).
* Melting: As the oceanic plate sinks, it gets heated by the mantle. This heat, combined with water released from the subducting plate, melts the surrounding mantle.
* Magma Formation: The molten rock, called magma, rises to the surface, often creating volcanoes.
* Volcanic Arc: These volcanoes often form a curved chain of mountains parallel to the subduction zone, known as a volcanic arc.
Examples of volcanic arcs:
* The Andes Mountains in South America
* The Cascade Range in North America
* The Japanese Islands
These mountain ranges are characterized by their volcanic activity and often contain large, towering peaks.
