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Isla Blanca (Sandwich del Sur)

Bristol Island

Estratovolcán · United Kingdom · 1100 m

The largely glacier-covered, 9 x 10 km Bristol Island is one of the largest of the South Sandwich Islands.  Both summit and flank vents on Bristol Island have been active during historical time.  The latest eruption, during 1956, originated from the west-flank crater, and deposited cinder over the icecap.  The extensive icecap on Bristol Island and the difficulty of landing make it the least explored of the South Sandwich Islands.
The largely glacier-covered, 9 x 10 km Bristol Island is one of the largest of the South Sandwich Islands. Both summit and flank vents on Bristol Island have been active during historical time. The latest eruption, during 1956, originated from the west-flank crater, and deposited cinder over the icecap. The extensive icecap on Bristol Island and the difficulty of landing make it the least explored of the South Sandwich Islands. · Foto: ASTER satellite image, 2002 (National Aeronautical and Space Administration, courtesy of ASTER science team). · Wikimedia Commons
Tipo
Estratovolcán
País
United Kingdom
Región
Antarctic-Scotia Volcanic Regions / South Sandwich Volcanic Arc
Altitud
1100 m
Coordenadas
-59.017, -26.533
Última erupción
2016
Contexto tectónico
Subduction zone / Oceanic crust (< 15 km)
Forma volcánica
Composite
Roca principal
Basalt / Picro-Basalt
Resumen geológico

The 9 x 10 km Bristol Island near the southern end of the South Sandwich arc lies across Fortser's Passage from the Southern Thule Islands and forms one of the largest islands of the chain. Largely glacier-covered, it contains a horseshoe-shaped ridge at the interior extending northward from the highest peak, 1100-m-high Mount Darnley. A steep-sided flank cone or lava dome, Havfruen Peak, is located on the east side, and a young crater and fissure are on the west flank. Three large sea stacks lying off Turmoil Point at the western tip of the island may be remnants of an older now-eroded volcanic center. Both summit and flank vents have been active during historical time. The latest eruption, during 1956, originated from the west-flank crater, and deposited cinder over the icecap. The extensive icecap and the difficulty of landing make it the least explored of the South Sandwich Islands.

Resumen de Wikipedia

La isla Blanco o isla Blanca es una pequeña isla deshabitada que integra el archipiélago de las Sandwich del Sur, en el mar del Scotia . Está situada entre la isla Jorge y el grupo Tule del Sur, del que está separada por el pasaje Forster.

Wikipedia · CC BY-SA · Leer artículo completo

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1823~1842 · 1 erupciones · VEI máx. 21920~1939 · 2 erupciones · VEI máx. 21939~1958 · 2 erupciones · VEI máx. 31997~2016 · 1 erupciones · VEI máx. 118231862192019581997

Línea de tiempo detallada

  1. 2016VEI 1Observado
    2016-04-24 – 2016-07-26
    Main crater, Mt. Sourabaya
  2. 1956VEI 3Observado
    1956-01-11 – 1956-01-19
    West flank
  3. 1950VEI 2Observado
    1950-03-27 – En curso
  4. 1936VEI 2Observado
    1936-12-18 – 1937-01-01
  5. 1935VEI 2Observado
    1935-12-31 – En curso
  6. 1823VEI 2Observado
    1823 – En curso

Enlaces externos

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