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Savo Island

Savo

Stratovolcano · 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. · Photo: Photo by Nick Varley (University of Colima). · Wikimedia Commons
Type
Stratovolcano
Country
Solomon Islands
Region
Southwestern Pacific Volcanic Regions / Solomon Volcanic Province
Elevation
455m
Coordinates
-9.132, 159.812
Last eruption
1847
Tectonic setting
Subduction zone / Crustal thickness unknown
Landform
Composite
Major rock type
Andesite / Basaltic Andesite
Geological summary

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.

Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
1568~1598 · 1 eruptions · max VEI 31627~1657 · 1 eruptions · max VEI ?1806~1835 · 1 eruptions · max VEI 31835~1865 · 1 eruptions · max VEI ?15681627171717761835

Detailed timeline

  1. 1865 (±20 yrs)VEI ?Geological estimate
    1865 – Ongoing
  2. 1835 (±5 yrs)VEI 3Observed
    1835 – 1847
  3. 1650 (±20 yrs)VEI ?Geological estimate
    1650 – Ongoing
  4. 1568VEI 3Observed
    1568 – Ongoing
    NE crater margin

External links

⚠ For reference only. Not for emergency response.