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Isla de Savo

Savo

Estratovolcán · Solomon Islands · 455 m

The 6 x 7 km island of Savo has been the source of major historical eruptions, which included pyroclastic flows that devastated much of the island. The summit contains a 1 x 1.5 km crater and lava domes are located on its floor, NE rim, and the outer flank of the volcano. Thermal areas located in the summit crater, along the flanks of the volcano, and offshore include fumaroles and small geysers.
The 6 x 7 km island of Savo has been the source of major historical eruptions, which included pyroclastic flows that devastated much of the island. The summit contains a 1 x 1.5 km crater and lava domes are located on its floor, NE rim, and the outer flank of the volcano. Thermal areas located in the summit crater, along the flanks of the volcano, and offshore include fumaroles and small geysers. · Foto: Photo by Nick Varley (University of Colima). · Wikimedia Commons
Tipo
Estratovolcán
País
Solomon Islands
Región
Pacífico Suroccidental / Solomon Volcanic Province
Altitud
455 m
Coordenadas
-9.132, 159.812
Última erupción
1847
Contexto tectónico
Subduction zone / Crustal thickness unknown
Forma volcánica
Composite
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

The 6 x 7 km island of Savo, off the NE coast of Guadalcanal Island, consists of a forested andesitic-to-dacitic stratovolcano with a shallow, elliptical 1 x 1.5 km summit crater. Young lava domes are located on the crater floor and the NE rim, and older domes occur on the flanks. Pyroclastic flows and mudflows traveled down valleys from the summit crater to form debris fans along the coast. Thermal areas located in the summit crater, the S to SE flanks, and offshore include areas of steaming ground, fumaroles, small geysers, and hot springs. Spanish explorers observed the first recorded eruption in 1568. Pyroclastic flows during the climactic phase killed almost all inhabitants of the island, and oral traditions also note the expansion of the island on the northern side. Other eruptive episodes occurred during the mid-17th century and during the 1830s to 1840s.

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1568~1598 · 1 erupciones · VEI máx. 31627~1657 · 1 erupciones · VEI máx. ?1806~1835 · 1 erupciones · VEI máx. 31835~1865 · 1 erupciones · VEI máx. ?15681627171717761835

Línea de tiempo detallada

  1. 1865 (±20 años)VEI ?Estimación geológica
    1865-07-02 – En curso
  2. 1835 (±5 años)VEI 3Observado
    1835-07-02 – 1847-07-02
  3. 1650 (±20 años)VEI ?Estimación geológica
    1650 – En curso
  4. 1568VEI 3Observado
    1568 – En curso
    NE crater margin

Enlaces externos

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