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Savo

성층화산 · Solomon Islands · 455m

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. · 사진: Photo by Nick Varley (University of Colima). · Wikimedia Commons
화산 유형
성층화산
국가
Solomon Islands
지역
Southwestern Pacific Volcanic Regions / Solomon Volcanic Province
해발
455m
좌표
-9.132, 159.812
마지막 분화
1847년
판구조 환경
Subduction zone / Crustal thickness unknown
화산 지형
Composite
주요 암석
Andesite / Basaltic Andesite
지질학적 요약

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.

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
1568~1598 · 1건 · 최고 VEI 31627~1657 · 1건 · 최고 VEI ?1806~1835 · 1건 · 최고 VEI 31835~1865 · 1건 · 최고 VEI ?15681627171717761835

상세 타임라인

  1. 1865년 (±20년)VEI ?지질학적 추정
    1865 ~ 진행 중
  2. 1835년 (±5년)VEI 3관측 기록
    1835 ~ 1847
  3. 1650년 (±20년)VEI ?지질학적 추정
    1650 ~ 진행 중
  4. 1568년VEI 3관측 기록
    1568 ~ 진행 중
    NE crater margin

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