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  2. Llaima - Wikipedia

    en.wikipedia.org/wiki/Llaima

    The top of Llaima consists of two summits; the lower of the two, Pichillaima, is about 2,920 m (9,580 ft) high and is significantly less prominent than the higher northern summit. [2] The average elevation of the terrain around Llaima is about 740 m asl. [2] The volcano summit is located 10 km West South West of Conguillío Lake.

  3. Conguillío National Park - Wikipedia

    en.wikipedia.org/wiki/Conguillío_National_Park

    Llaima volcano was formed during the Quaternary, on lava and granites located throughout the faults system of longitudinal North – South. It is composed of mixed volcano and shield, with a boiler covered with forty accidental dreg cones and presents a secondary chimney to 9.514,44 feet above the sea level. The slope of this volcano is moderate.

  4. List of volcanoes in Chile - Wikipedia

    en.wikipedia.org/wiki/List_of_volcanoes_in_Chile

    The country's National Geology and Mining Service lists 90 active volcanoes. [2] The volcanoes of the Andes originate from the subduction of the Nazca Plate under the South American Plate, while the volcanoes of Chile's Pacific islands formed from magma coming from three distinct hotspots, Easter, Juan Fernández and San Felix hotspots. The ...

  5. Melipeuco - Wikipedia

    en.wikipedia.org/wiki/Melipeuco

    Melipeuco (Spanish pronunciation: [meliˈpewko]) is a town and commune (Spanish: comuna) in Chile, located at the foot of the Andes, in the Province of Cautín, Araucanía Region. Melipeuco is 12 km (7 mi) from the southern entrance of the Conguillío National Park .

  6. Temuco - Wikipedia

    en.wikipedia.org/wiki/Temuco

    Temuco is located in a valley in the center-south of Chile, equidistant between the Pacific Ocean to the west and the Andes to the east. Morphologically , the city placement corresponds to Cautín River -originated fluvial land masses that developed in a crushed form between two hills, Ñielol (350m) and Conunhueno (360m).

  7. Geology of Chile - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Chile

    Llaima volcano in eruption. The geology of Chile is a characterized by processes linked to subduction, such as volcanism, earthquakes, and orogeny.The building blocks of Chile's geology were assembled during the Paleozoic Era when Chile was the southwestern margin of the supercontinent Gondwana.

  8. Ring of Fire - Wikipedia

    en.wikipedia.org/wiki/Ring_of_Fire

    The Llaima Volcano is one of the largest and most active volcanoes in Chile. It is situated 82 km (51 mi) northeast of Temuco and 663 km (412 mi) southeast of Santiago, within the borders of Conguillío National Park. Llaima's activity has been documented since the 17th century, and consists of several separate episodes of moderate explosive ...

  9. Kütralkura - Wikipedia

    en.wikipedia.org/wiki/Kütralkura

    View of Conguillío Lake and Llaima Volcano, both part of Kütralkura Geopark. Kütralkura (Spanish: Geoparque Kütralkura, from Mapudungun kütral, fire, and kura, stone, meaning "firestone" [1]) is a geopark in southern Chile's Araucanía Region. The geopark has an area of 8100 km 2 and lies mostly in the Andes.