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Monte Erebus

Erebus

Estratovolcán · Antarctica · 3794 m

Mount Erebus is seen here from the SW near the McMurdo research station on Ross Island and the world's southernmost active volcano. The summit has a 500 x 600 m wide, 110-m-deep crater that contains an active lava lake. The glaciated volcano was erupting when first sighted by Captain James Ross in 1841. Continuous lava lake activity has been documented since 1972, punctuated by occasional Strombolian explosions that eject bombs onto the crater rim.
Mount Erebus is seen here from the SW near the McMurdo research station on Ross Island and the world's southernmost active volcano. The summit has a 500 x 600 m wide, 110-m-deep crater that contains an active lava lake. The glaciated volcano was erupting when first sighted by Captain James Ross in 1841. Continuous lava lake activity has been documented since 1972, punctuated by occasional Strombolian explosions that eject bombs onto the crater rim. · Foto: Photo by Richard Waitt, 1972 (U.S. Geological Survey). · Wikimedia Commons
Tipo
Estratovolcán
País
Antarctica
Región
Antarctic-Scotia Volcanic Regions / McMurdo Volcanic Province
Altitud
3794 m
Coordenadas
-77.530, 167.170
Última erupción
2026
Contexto tectónico
Intraplate / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Phonolite
Resumen geológico

Mount Erebus overlooks the McMurdo research station on Ross Island and is the largest of three major volcanoes forming the roughly triangular Ross Island. The summit of the dominantly phonolitic volcano has been modified by one or two generations of caldera formation. A summit plateau at about 3,200 m elevation marks the rim of the youngest caldera, which formed during the late-Pleistocene and within which the modern cone was constructed. An elliptical 500 x 600 m, 110-m-deep crater truncates the summit and contains an active lava lake within a 250-m-wide, 100-m-deep inner crater; other lava lakes are sometimes present. The glacier-covered volcano was erupting when first sighted by Captain James Ross in 1841. A persistent lava-lake, with minor explosions punctuated by occasional larger Strombolian explosions that eject bombs onto the crater rim, has been documented since 1972, but nearly continuous activity has probably been occurring for much longer.

Resumen de Wikipedia

El monte Erebus, en la Antártica, es el volcán activo más austral de la Tierra. Tiene una altitud de 3794 metros y está localizado en la isla de Ross, que también tiene otros tres volcanes activos, entre ellos el monte Terror. Esta montaña forma parte del cinturón de fuego del Pacífico, que incluye 1600 volcanes activos.

Wikipedia · CC BY-SA · Leer artículo completo

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
8050 BCE~7716 BCE · 1 erupciones · VEI máx. 07382 BCE~7048 BCE · 1 erupciones · VEI máx. 04709 BCE~4375 BCE · 1 erupciones · VEI máx. 04375 BCE~4041 BCE · 1 erupciones · VEI máx. 03039 BCE~2705 BCE · 1 erupciones · VEI máx. 02371 BCE~2037 BCE · 1 erupciones · VEI máx. 0636~970 · 1 erupciones · VEI máx. 01638~1972 · 15 erupciones · VEI máx. 28050 BCE5712 BCE3039 BCE701 BCE1638

Línea de tiempo detallada

  1. 1972VEI 1Observado
    1972-01-03 – En curso
  2. 1972VEI 2Observado
    1972-12-16 – 2026-03-17
  3. 1963VEI 0Observado
    1963-11-16 – En curso
  4. 1957VEI ?Estimación geológica
    1957-07-02 – 1958-07-02
  5. 1955VEI 2Observado
    1955-07-02 – En curso
  6. 1947VEI 2Observado
    1947-02 – En curso
  7. 1915VEI 2Observado
    1915-03-22 – En curso
  8. 1915VEI 2Observado
    1915-08 – En curso
  9. 1912VEI 2Observado
    1912-12-12 – En curso
  10. 1911VEI 2Observado
    1911-04 – 1911-06
  11. 1911VEI 2Observado
    1911-10 – En curso
  12. 1908VEI 2Observado
    1908-03 – 1908-11
  13. 1903VEI 0Observado
    1903-01-01 – En curso
  14. 1900VEI 2Estimación geológica
    1900-02 – En curso
  15. 1841VEI 1Observado
    1841-01-28 – 1841-02
  16. 950 (±4000 años)VEI 0Estimación geológica
    950 – En curso
  17. 2050 a. C. (±3000 años)VEI 0Estimación geológica
    BCE 2050 – En curso
    Western Crater (Upper Ice Tower flow)
  18. 2950 a. C. (±300 años)VEI 0Estimación geológica
    BCE 2950 – En curso
    North flank (Lower Hut lava flow)
  19. 4050 a. C. (±500 años)VEI 0Estimación geológica
    BCE 4050 – En curso
    Lower Ice Tower Ridge, S lava flows
  20. 4550 a. C. (±500 años)VEI 0Estimación geológica
    BCE 4550 – En curso
    NE flank
  21. 7050 a. C. (±2000 años)VEI 0Estimación geológica
    BCE 7050 – En curso
    NW flank
  22. 8050 a. C. (±5000 años)VEI 0Estimación geológica
    BCE 8050 – En curso
    NNW flank

Enlaces externos

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