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Savo Island

Savo

Stratovolkan · 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
Tipe
Stratovolkan
Negara
Solomon Islands
Wilayah
Southwestern Pacific Volcanic Regions / Solomon Volcanic Province
Ketinggian
455 m
Koordinat
-9.132, 159.812
Letusan terakhir
1847
Kondisi tektonik
Subduction zone / Crustal thickness unknown
Bentuk lahan
Composite
Batuan utama
Andesite / Basaltic Andesite
Ringkasan geologi

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.

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
1568~1598 · 1 letusan · VEI maks. 31627~1657 · 1 letusan · VEI maks. ?1806~1835 · 1 letusan · VEI maks. 31835~1865 · 1 letusan · VEI maks. ?15681627171717761835

Garis waktu rinci

  1. 1865 (±20 tahun)VEI ?Perkiraan geologi
    1865 – Berlangsung
  2. 1835 (±5 tahun)VEI 3Teramati
    1835 – 1847
  3. 1650 (±20 tahun)VEI ?Perkiraan geologi
    1650 – Berlangsung
  4. 1568VEI 3Teramati
    1568 – Berlangsung
    NE crater margin

Tautan eksternal

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