Report on Raung (Indonesia) — November 1985
Scientific Event Alert Network Bulletin, vol. 10, no. 11 (November 1985)
Managing Editor: Lindsay McClelland.
Raung (Indonesia) Many small explosions; light ashfalls
Please cite this report as:
Global Volcanism Program, 1985. Report on Raung (Indonesia). In: McClelland, L (ed.), Scientific Event Alert Network Bulletin, 10:11. Smithsonian Institution. https://doi.org/10.5479/si.GVP.SEAN198511-263340.
8.119°S, 114.056°E; summit elev. 3260 m
All times are local (unless otherwise noted)
"Raung resumed activity during November with a series of small explosions. The summit crater has not been visited since the start of the latest activity. However, observations begun 1 November from the new Raung observation post about 15 km SE of the summit at 700 m altitude (at Mangaran) indicated that the explosions have been centered along the E side of the large summit crater, near the recently active eruptive vent on the crater floor. At least 44 explosion clouds were observed during November, mostly whitish in color but dark gray ash-laden clouds were also seen. On 15 November, light ashfall was reported from SE flank villages (Bejong, Mangaran, and Seragi) and from Banjuyangi City, 35 km ESE of the volcano. The Mangaran seismometer recorded 52 explosion earthquakes during November. Activity was continuing as of 12 December."
"The last eruption of Raung that produced a lava flow was in 1973. That flow was confined to the summit crater. Explosions similar to the November activity have frequently been reported over the last decade."
Geologic Background. Raung, one of Java's most active volcanoes, is a massive stratovolcano in easternmost Java that was constructed SW of the rim of Ijen caldera. The unvegetated summit is truncated by a dramatic steep-walled, 2-km-wide caldera that has been the site of frequent historical eruptions. A prehistoric collapse of Gunung Gadung on the W flank produced a large debris avalanche that traveled 79 km, reaching nearly to the Indian Ocean. Raung contains several centers constructed along a NE-SW line, with Gunung Suket and Gunung Gadung stratovolcanoes being located to the NE and W, respectively.
Information Contacts: T. Casadevall and L. Pardyanto, VSI; Antara News Service, Jakarta.