Report on Lewotolo (Indonesia) — 28 July-3 August 2004
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 28 July-3 August 2004
Managing Editor: Gari Mayberry
Please cite this report as:
Global Volcanism Program, 2004. Report on Lewotolo (Indonesia). In: Mayberry, G (ed.), Weekly Volcanic Activity Report, 28 July-3 August 2004. Smithsonian Institution and US Geological Survey.
8.272°S, 123.505°E; summit elev. 1423 m
All times are local (unless otherwise noted)
DVGHM stated that the pilot report of a plume emitted from Lewotolo on 25 June was false. Further investigation revealed that the emission was actually from Egon.
Geologic Background. Anchoring the eastern end of an elongated peninsula that is connected to Lembata (formerly Lomblen) Island by a narrow isthmus and extends northward into the Flores Sea, Lewotolo rises to 1423 m. Lewotolo is a symmetrical stratovolcano as viewed from the north and east. A small cone with a 130-m-wide crater constructed at the SE side of a larger crater forms the volcano's high point. Many lava flows have reached the coastline. Historical eruptions, recorded since 1660, have consisted of explosive activity from the summit crater.