Report on Barren Island (India) — 1 June-7 June 2005
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 1 June-7 June 2005
Managing Editor: Gari Mayberry
Please cite this report as:
Global Volcanism Program, 2005. Report on Barren Island (India). In: Mayberry, G (ed.), Weekly Volcanic Activity Report, 1 June-7 June 2005. Smithsonian Institution and US Geological Survey.
12.278°N, 93.858°E; summit elev. 354 m
All times are local (unless otherwise noted)
Professor Chandrasekharam, from the Indian Institute of Technology, reported that the volcanic activity that began at Barren Island on 28 May continued through 6 June when fresh lava emissions were observed by the Indian Coast Guard. Large amounts of steam were emitted due to the interaction of heavy rains and the hot lava.
According to Dhanapati Haldar, from the Presidency College, Strombolian activity on Barren Island consisted of lava fountaining to a height of ~100 m and "dark smoke" rising to ~1 km above the volcano. Lava accumulated on the W side of the main volcanic cone.
Geologic Background. Barren Island, a possession of India in the Andaman Sea about 135 km NE of Port Blair in the Andaman Islands, is the only historically active volcano along the N-S volcanic arc extending between Sumatra and Burma (Myanmar). It is the emergent summit of a volcano that rises from a depth of about 2250 m. The small, uninhabited 3-km-wide island contains a roughly 2-km-wide caldera with walls 250-350 m high. The caldera, which is open to the sea on the west, was created during a major explosive eruption in the late Pleistocene that produced pyroclastic-flow and -surge deposits. Historical eruptions have changed the morphology of the pyroclastic cone in the center of the caldera, and lava flows that fill much of the caldera floor have reached the sea along the western coast.
Sources: Professor Chandrasekharam from the Indian Institute of Technology, Dhanapati Haldar, Presidency College