Report on Yasur (Vanuatu) — 13 November-19 November 2013
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 13 November-19 November 2013
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2013. Report on Yasur (Vanuatu). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 13 November-19 November 2013. Smithsonian Institution and US Geological Survey.
19.53°S, 169.442°E; summit elev. 361 m
All times are local (unless otherwise noted)
On 19 November, the Vanuatu Geohazards Observatory reported that a new phase of ash emissions from Yasur began on 3 November. The intensity of the explosive activity remained low; therefore the Alert Level remained at 1 (on a scale of 0-4).
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: Vanuatu Geohazards Observatory