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Volcán Antuco

Antuco

Estratovolcán · Chile · 2979 m

Antuco volcano, seen here from the NW, has a complicated history beginning with construction of an andesitic stratovolcano during the Pleistocene.  Edifice failure at the beginning of the Holocene produced a large debris avalanche that traveled down the Río Laja to the west.  The collapse left a large horseshoe-shaped caldera whose NW rim forms the ridge descending to the right.  The steep-sided modern basaltic cone (upper right) has grown 1000 m since then.  Moderate explosive eruptions were recorded in the 18th and 19th centuries.
Antuco volcano, seen here from the NW, has a complicated history beginning with construction of an andesitic stratovolcano during the Pleistocene. Edifice failure at the beginning of the Holocene produced a large debris avalanche that traveled down the Río Laja to the west. The collapse left a large horseshoe-shaped caldera whose NW rim forms the ridge descending to the right. The steep-sided modern basaltic cone (upper right) has grown 1000 m since then. Moderate explosive eruptions were recorded in the 18th and 19th centuries. · Foto: Photo by Norm Banks, 1990 (U.S. Geological Survey). · Wikimedia Commons
Tipo
Estratovolcán
País
Chile
Región
South America Volcanic Regions / Southern Andean Volcanic Arc
Altitud
2979 m
Coordenadas
-37.406, -71.349
Última erupción
1869
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Basalt / Picro-Basalt
Resumen geológico

Antuco volcano, constructed NE of the Pleistocene Sierra Velluda stratovolcano, rises dramatically above the SW shore of Laguna de la Laja. It has a complicated history beginning with construction of the basaltic-to-andesitic Sierra Velluda and Cerro Condor stratovolcanoes of Pliocene-Pleistocene age. Construction of the Antuco I volcano was followed by edifice failure at the beginning of the Holocene that produced a large debris avalanche which traveled down the Río Laja to the west and left a large 5-km-wide caldera breached to the west. The steep-sided modern basaltic-to-andesitic cone has grown 1,000 m since then; flank fissures and cones have also been active. Moderate explosive eruptions were recorded in the 18th and 19th centuries from both summit and flank vents, and lava flows have traveled into the Río Laja drainage.

Resumen de Wikipedia

El volcán Antuco es un estratovolcán ubicado en la comuna homónima, región del Bío-Bío, Chile. Se encuentra dentro del parque nacional Laguna del Laja, en la ribera suroeste de la laguna Laja, a noventa kilómetros al este de Los Ángeles.

Wikipedia · CC BY-SA · Leer artículo completo

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
7750 BCE~7429 BCE · 1 erupciones · VEI máx. ?1548~1869 · 13 erupciones · VEI máx. 37750 BCE5506 BCE2940 BCE696 BCE1548

Línea de tiempo detallada

  1. 1869VEI 2Observado
    1869 – En curso
  2. 1863VEI 2Observado
    1863-12 – En curso
  3. 1862VEI ?Estimación geológica
    1862-01 – 1862-03-03
  4. 1861VEI 0Observado
    1861-02 – 1861-08
  5. 1852VEI 3Observado
    1852-11 – 1853-01
    NE flank fissure and summit
  6. 1848VEI 2Estimación geológica
    1848 – En curso
  7. 1845VEI 2Observado
    1845-02-26 – 1845-03-01
  8. 1839VEI 2Estimación geológica
    1839 – En curso
  9. 1828VEI 2Observado
    1828-12-18 – En curso
  10. 1820VEI 1Observado
    1820 – 1821
  11. 1806VEI 2Observado
    1806-05 – En curso
  12. 1752VEI 3Observado
    1752-01-31 – 1752-02-01
  13. 1750 (±10 años)VEI 2Observado
    1750 – En curso
  14. 7750 a. C.VEI ?Estimación geológica
    BCE 7750 – En curso

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.