Llaima Volcano, located in Chile, is not classified as a hotspot but rather as a stratovolcano formed by subduction processes at the boundary of the Nazca and South American tectonic plates. Hotspots are typically associated with volcanic activity that occurs away from tectonic plate boundaries, such as the Hawaiian Islands. Llaima is part of the Andes mountain range, which is characterized by volcanic activity due to the ongoing subduction of the Nazca Plate beneath the South American Plate.
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