The mountains on the west coasts of North and South America, such as the Rocky Mountains and the Andes, are primarily the result of tectonic plate interactions. The subduction of the Nazca Plate beneath the South American Plate causes volcanic activity and mountain formation in the Andes, while the collision and uplift of various tectonic plates contribute to the Rockies' formation. These geological processes create dramatic landscapes and are driven by the ongoing movement of Earth's tectonic plates.
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