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Volcán Hudson

Hudson, Cerro

Estratovolcán · Chile · 1905 m

The ice-filled 10-km-wide caldera of the remote Cerro Hudson volcano was not recognized until its first 20th-century eruption in 1971.  The massive, 1905-m-high Cerro Hudson, seen here from the west on August 23 during its 1991 eruption, covers an area of 300 km2.  The caldera is drained through a breach on its NW rim (upper left), which has been the source of mudflows down the Rio de Los Huemules.  The 1991 eruption was Chile's second largest of the 20th century, and formed a new 800-m-wide crater in the SW part of the caldera.
The ice-filled 10-km-wide caldera of the remote Cerro Hudson volcano was not recognized until its first 20th-century eruption in 1971. The massive, 1905-m-high Cerro Hudson, seen here from the west on August 23 during its 1991 eruption, covers an area of 300 km2. The caldera is drained through a breach on its NW rim (upper left), which has been the source of mudflows down the Rio de Los Huemules. The 1991 eruption was Chile's second largest of the 20th century, and formed a new 800-m-wide crater in the SW part of the caldera. · Foto: Photo by Norm Banks, 1991 (U.S. Geological Survey). · Wikimedia Commons
Tipo
Estratovolcán
País
Chile
Región
South America Volcanic Regions / Southern Andean Volcanic Arc
Altitud
1905 m
Coordenadas
-45.900, -72.970
Última erupción
2011
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Basalt / Picro-Basalt
Resumen geológico

The ice-filled, 10-km-wide caldera of Cerro Hudson volcano was not recognized until its first 20th-century eruption in 1971. It is the southernmost volcano in the Chilean Andes, related to subduction of the Nazca plate beneath the South American plate. The massive volcano covers an area of 300 km2. The compound caldera is drained through a breach on its NW rim, which has been the source of mudflows down the Río de Los Huemeles. Two cinder cones occur N of the volcano and others occupy the SW and SE flanks. This volcano has been the source of several major Holocene explosive eruptions. An eruption about 6,700 years ago was one of the largest known in the southern Andes during the Holocene; another eruption about 3,600 years ago also produced more than 10 km3 of tephra. An eruption in 1991 formed a new 800-m-wide crater in the SW portion of the caldera.

Resumen de Wikipedia

El volcán Hudson o monte Hudson es un volcán chileno ubicado a 15 kilómetros del océano Pacífico y a 62 kilómetros al sur de Coyhaique, al sur del Puerto Aysén y al norte de los Campos de Hielo Norte, en la región de Aysén del General Carlos Ibáñez del Campo.

Wikipedia · CC BY-SA · Leer artículo completo

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
8010 BCE~7676 BCE · 1 erupciones · VEI máx. ?5004 BCE~4670 BCE · 2 erupciones · VEI máx. 64002 BCE~3668 BCE · 1 erupciones · VEI máx. ?2331 BCE~1997 BCE · 1 erupciones · VEI máx. ?1997 BCE~1663 BCE · 1 erupciones · VEI máx. 6995 BCE~661 BCE · 1 erupciones · VEI máx. ?327 BCE~7 · 1 erupciones · VEI máx. ?341~675 · 1 erupciones · VEI máx. ?675~1009 · 1 erupciones · VEI máx. ?1677~2011 · 5 erupciones · VEI máx. 58010 BCE5672 BCE2999 BCE661 BCE1677

Línea de tiempo detallada

  1. 2011VEI 2Observado
    2011-10-26 – 2011-11-01
    S and SE edge of the caldera
  2. 1991VEI 5Observado
    1991-08-08 – 1991-10-27
    NW caldera rim and SW caldera floor
  3. 1971VEI 3Observado
    1971-08-12 – 1971-09-18
    NW part of caldera
  4. 1891VEI ?Observado
    1891 – En curso
  5. 1740 (±150 años)VEI ?Estimación geológica
    1740 – En curso
  6. 860 (±100 años)VEI ?Estimación geológica
    860 – En curso
  7. 390 (±150 años)VEI ?Estimación geológica
    390 – En curso
  8. 120 a. C. (±200 años)VEI ?Estimación geológica
    BCE 120 – En curso
  9. 790 a. C. (±75 años)VEI ?Estimación geológica
    BCE 790 – En curso
  10. 1890 a. C.VEI 6Estimación geológica
    BCE 1890 – En curso
  11. 2250 a. C.VEI ?Estimación geológica
    BCE 2250 – En curso
  12. 3890 a. C. (±500 años)VEI ?Estimación geológica
    BCE 3890 – En curso
  13. 4750 a. C.VEI 6Estimación geológica
    BCE 4750 – En curso
  14. 4960 a. C. (±150 años)VEI ?Estimación geológica
    BCE 4960 – En curso
  15. 8010 a. C.VEI ?Estimación geológica
    BCE 8010 – En curso

Enlaces externos

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