Report on Yasur (Vanuatu) — 23 January-29 January 2002

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 23 January-29 January 2002
Managing Editor: Gari Mayberry

Please cite this report as:

Global Volcanism Program, 2002. Report on Yasur (Vanuatu). In: Mayberry, G (ed.), Weekly Volcanic Activity Report, 23 January-29 January 2002. Smithsonian Institution and US Geological Survey.

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Yasur

Vanuatu

19.53°S, 169.442°E; summit elev. 361 m

All times are local (unless otherwise noted)


An eruption occurred at Yasur on 25 January around 1300. A pilot reported that an ash cloud rose ~2 km a.s.l. and slowly drifted S. The ash cloud was not visible on satellite imagery, possibly due to heavy meteorological cloud cover.

Geologic Background. Yasur, the best-known and most frequently visited of the Vanuatu volcanoes, has been in more-or-less continuous strombolian and vulcanian activity since Captain Cook observed ash eruptions in 1774. This style of activity may have continued for the past 800 years. Located at the SE tip of Tanna Island, this mostly unvegetated pyroclastic cone has a nearly circular, 400-m-wide summit crater. Yasur is largely contained within the small Yenkahe caldera and is the youngest of a group of Holocene volcanic centers constructed over the down-dropped NE flank of the Pleistocene Tukosmeru volcano. The Yenkahe horst is located within the Siwi ring fracture, a 4-km-wide, horseshoe-shaped caldera associated with eruption of the andesitic Siwi pyroclastic sequence. Active tectonism along the Yenkahe horst accompanying eruptions has raised Port Resolution harbor more than 20 m during the past century.

Source: Wellington Volcanic Ash Advisory Center (VAAC)