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Report on White Island (New Zealand) — 19 December-25 December 2012

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 19 December-25 December 2012
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2012. Report on White Island (New Zealand). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 19 December-25 December 2012. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (19 December-25 December 2012)

White Island

New Zealand

37.52°S, 177.18°E; summit elev. 294 m

All times are local (unless otherwise noted)

On 20 December, GeoNet Data Centre reported that the spiny lava dome at White Island had not changed during the previous 10 days. No changes to the lava dome were noted when scientists compared photos taken on 19 December to previous ones, but several small lakes occupied parts of where a large lake was before August. The highest temperature reading from the lava dome was 187 degrees Celsius, the hot lake to the S was at least 71 degrees and upwelling strongly, and the cool lake on the N side of the dome was 35 degrees. The Alert Level remained at 2 (on a scale of 0-5), and the Aviation Colour Code remained at Orange (second highest on a four-color scale).

Geologic Background. The uninhabited White Island, also known as Whakaari in the Maori language, is the 2 x 2.4 km emergent summit of a 16 x 18 km submarine volcano in the Bay of Plenty about 50 km offshore of North Island. The island consists of two overlapping andesitic-to-dacitic stratovolcanoes. The summit crater appears to be breached to the SE, because the shoreline corresponds to the level of several notches in the SE crater wall. Volckner Rocks, sea stacks that are remnants of a lava dome, lie 5 km NW. Descriptions of eruptions since 1826 have included intermittent moderate phreatic, phreatomagmatic, and Strombolian eruptions; activity there also forms a prominent part of Maori legends. Formation of many new vents during the 19th and 20th centuries has produced rapid changes in crater floor topography. Collapse of the crater wall in 1914 produced a debris avalanche that buried buildings and workers at a sulfur-mining project. Explosive activity in December 2019 took place while tourists were present, resulting in many fatalities.

Source: GeoNet