Report on Yasur (Vanuatu) — March 1986
Scientific Event Alert Network Bulletin, vol. 11, no. 3 (March 1986)
Managing Editor: Lindsay McClelland
Yasur (Vanuatu) Frequent small Strombolian explosions
Please cite this report as:
Global Volcanism Program, 1986. Report on Yasur (Vanuatu). In: McClelland, L (ed.), Scientific Event Alert Network Bulletin, 11:3. Smithsonian Institution. http://dx.doi.org/10.5479/si.GVP.SEAN198603-257100.
19.53°S, 169.442°E; summit elev. 361 m
All times are local (unless otherwise noted)
"[On 4 March] there were three aligned craters, perhaps 300 m apart . . ., heavy fumarolic activity occurred from the northernmost crater. Frequent noisy Strombolian activity ejected tephra to heights of tens of meters from the other two craters. Tephra did not rise above the volcano's summit."
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.
Information Contacts: R. Stoiber, Dartmouth College.