Report on Batur (Indonesia) — 17 November-23 November 2010
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 17 November-23 November 2010
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2010. Report on Batur (Indonesia). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 17 November-23 November 2010. Smithsonian Institution and US Geological Survey.
8.242°S, 115.375°E; summit elev. 1717 m
All times are local (unless otherwise noted)
CVGHM reported that seismicity from Batur decreased from 1 June to 17 November and fumarolic plumes rose from the crater. On 19 November the Alert level was lowered to Normal, or 1 (on a scale of 1-4).
Geologic Background. The historically active Batur is located at the center of two concentric calderas NW of Agung volcano. The outer 10 x 13.5 km wide caldera was formed during eruption of the Bali (or Ubud) Ignimbrite about 29,300 years ago and now contains a caldera lake on its SE side, opposite the satellitic Gunung Abang cone, the topographic high of the complex. The inner 6.4 x 9.4 km wide caldera was formed about 20,150 years ago during eruption of the Gunungkawi Ignimbrite. The SE wall of the inner caldera lies beneath Lake Batur; Batur cone has been constructed within the inner caldera to a height above the outer caldera rim. The Batur stratovolcano has produced vents over much of the inner caldera, but a NE-SW fissure system has localized the Batur I, II, and III craters along the summit ridge. Historical eruptions have been characterized by mild-to-moderate explosive activity sometimes accompanied by lava emission. Basaltic lava flows from both summit and flank vents have reached the caldera floor and the shores of Lake Batur in historical time.