The Vanuatu Geohazards Observatory reported that the Vanuatu Volcano Alert Level (VVAL) for Yasur was increased to 3 (on a scale of 0-4) on 27 May. Recent activity was characterized by moderate to large eruptions with strong explosions, ejected bombs that fell on the visitor viewing area, and significant ashfall in nearby villages. Visitors were not allowed to enter a restricted zone, within about 500 m around the volcano. Activity had been escalating since January 2010. According to a news article, an eruption plume on 1 June rose to an altitude of 1.8 km (6,000 ft) a.s.l. and spread over 340 square kilometers, canceling or delaying some flights in and out of New Caledonia (about 430 km WSW).

Geological Summary. Yasur has exhibited essentially continuous Strombolian and Vulcanian activity at least 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 in Vanuatu, this pyroclastic cone has a nearly circular, 400-m-wide summit crater. The active cone 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 open feature 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.

Sources: Vanuatu Meteorology and Geohazards Department (VMGD), Agence France-Presse (AFP), Notimex