Increased seismicity, steam and gas emissions at Savo volcano, Solomon Islands

Increased seismicity and gas and ash emissions were observed at Savo volcano, Solomon Islands at the end of July, prompting authorities to deploy technical teams, increase monitoring and issue Volcano Safety Messages to residents. 

• Savo has been the source of major historical eruptions, which included pyroclastic flows that devastated much of the island. 
• The last eruption at this volcano took place in 1847 (VEI 3).

A team from the country's Geological Survey Division (GSD) and National Disaster Management Office (NDMO) investigated the volcano on July 30, 2021, following reports of increased seismicity and loud explosions on July 28.

The team saw steam and gas emissions rising from one area of the crater, possibly indicating an active fissure, and interviewed local residents.

"The GSD notified National Disaster Operations Committee and other authorities on July 31, confirming the increased seismicity, and prompting a preparedness response," USGS Volcanologist Sally Sennert noted. "The measures included further monitoring of the island, sending technical teams, and issuing Volcano Safety Messages to residents of the island and surrounding areas."¹

"I suspect some sort of steam blast from that site because people report seeing some sort of cloud above the area," Chief Geological Officer Thomas Toba told ABC.²

Image credit: Copernicus EU/Sentinel-2, TW. Acquired July 29, 2021

Savo Island, Solomon Islands on August 3, 2021. Image credit: Copernicus EU/Sentinel-2, TW

While volcanic activity on Savo has since subsided, Toba said Savo's proximity to Honiara makes it a constant worry for officials, especially in the case of a large eruption.

"Depending on the conditions of weather, at the time of eruption and the height of a column, and the size of eruption [it would] definitely affect the whole of Solomon Islands," he said.

Officials have asked experts from Vanuatu and Papua New Guinea for assistance in monitoring volcanic activity.

 

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Geological summary

The 6 x 7 km (3.7 x 4.3 miles) island of Savo consists of a forested andesitic-to-dacitic stratovolcano with a shallow, elliptical 1 x 1.5 km (0.6 x 0.9 miles) wide summit crater.

Lava domes of historical age are located on the crater floor and its NE rim, and older domes occur on the flanks of the volcano.

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 south to SE flanks, and offshore include areas of steaming ground, fumaroles, small geysers, and hot springs.

Spanish explorers arrived in 1568 during the first historical eruption of Savo. 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-17^th century and during the 1830s to 1840s.³

References:

¹ Global Volcanism Program, 2021. Report on Savo (Solomon Islands). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 28 July-3 August 2021. Smithsonian Institution and US Geological Survey – GVP.

² Solomon Islands seek regional help to monitor volcanic activity – ABC Radio Australia

³ Savo volcano, Solomon Islands – GVP

Featured image: Savo Island, Solomon Islands on August 3, 2021. Image credit: Copernicus EU/Sentinel-2, TW