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Report on Nevados de Chillan (Chile) — 27 November-3 December 2019

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 27 November-3 December 2019
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2019. Report on Nevados de Chillan (Chile). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 27 November-3 December 2019. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (27 November-3 December 2019)


Nevados de Chillan

Chile

36.868°S, 71.378°W; summit elev. 3180 m

All times are local (unless otherwise noted)


SERNAGEOMIN reported that during 26 November-3 December white-to-gray plumes from Nevados de Chillán’s Nicanor Crater rose as high as 1.7 km above the rim and drifted SE, NE, and NNW. Occasional explosions ejecting incandescent material onto the flank were visible at night. The report noted that the newest lava flow (L4) traveled down the NNE flank adjacent to three previous flows (L1, L2, and L3). The point of emission of L4 was about 60 m SSE of the emission point for the previous three lava flows. L4 had two lobes and was about 90 m long, measured from the rim of Nicanor Crater, on 27 November. By 29 November it had lengthened to 165 m. The volcano Alert Level remained at Orange, the second highest level on a four-color scale. ONEMI maintained an Alert Level Yellow (the middle level on a three-color scale) for the communities of Pinto, Coihueco, and San Fabián, and stated that the public should stay at least 3 km away from the crater on the SW flank and 5 km away on the ENE flank.

Geologic Background. The compound volcano of Nevados de Chillán is one of the most active of the Central Andes. Three late-Pleistocene to Holocene stratovolcanoes were constructed along a NNW-SSE line within three nested Pleistocene calderas, which produced ignimbrite sheets extending more than 100 km into the Central Depression of Chile. The largest stratovolcano, dominantly andesitic, Cerro Blanco (Volcán Nevado), is located at the NW end of the group. Volcán Viejo (Volcán Chillán), which was the main active vent during the 17th-19th centuries, occupies the SE end. The new Volcán Nuevo lava-dome complex formed between 1906 and 1945 between the two volcanoes and grew to exceed Volcán Viejo in elevation. The Volcán Arrau dome complex was constructed SE of Volcán Nuevo between 1973 and 1986 and eventually exceeded its height.

Source: Servicio Nacional de Geología y Minería (SERNAGEOMIN)