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Report on Lascar (Chile) — 3 April-9 April 2013

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 3 April-9 April 2013
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2013. Report on Lascar (Chile). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 3 April-9 April 2013. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (3 April-9 April 2013)


Lascar

Chile

23.37°S, 67.73°W; summit elev. 5592 m

All times are local (unless otherwise noted)


OVDAS-SERNAGEOMIN reported that during March a web camera monitoring Láscar recorded white gas plumes rising 600 m above the crater. At night during 2-4 April incandescence from the crater was observed. On 3 April increased emissions from the crater fluctuated from white to gray, indicating possible ash. Plumes rose 320 m and drifted SE. Seismicity remained at normal levels during the increased emissions. On 5 April the Alert Level was raised to Yellow.

Geologic Background. Láscar is the most active volcano of the northern Chilean Andes. The andesitic-to-dacitic stratovolcano contains six overlapping summit craters. Prominent lava flows descend its NW flanks. An older, higher stratovolcano 5 km E, Volcán Aguas Calientes, displays a well-developed summit crater and a probable Holocene lava flow near its summit (de Silva and Francis, 1991). Láscar consists of two major edifices; activity began at the eastern volcano and then shifted to the western cone. The largest eruption took place about 26,500 years ago, and following the eruption of the Tumbres scoria flow about 9000 years ago, activity shifted back to the eastern edifice, where three overlapping craters were formed. Frequent small-to-moderate explosive eruptions have been recorded since the mid-19th century, along with periodic larger eruptions that produced ashfall hundreds of kilometers away. The largest historical eruption took place in 1993, producing pyroclastic flows to 8.5 km NW of the summit and ashfall in Buenos Aires.

Source: Servicio Nacional de Geología y Minería (SERNAGEOMIN)