Savo Island
Savo
Stratovolkan · Solomon Islands · 455 m
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- 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
Garis waktu rinci
- 1865 (±20 tahun)VEI ?Perkiraan geologi1865 – Berlangsung
- 1835 (±5 tahun)VEI 3Teramati1835 – 1847
- 1650 (±20 tahun)VEI ?Perkiraan geologi1650 – Berlangsung
- 1568VEI 3Teramati1568 – BerlangsungNE crater margin
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.