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Report on Colima (Mexico) — 4 November-10 November 2015

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 4 November-10 November 2015
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2015. Report on Colima (Mexico). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 4 November-10 November 2015. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (4 November-10 November 2015)


Colima

Mexico

19.514°N, 103.62°W; summit elev. 3850 m

All times are local (unless otherwise noted)


Based on satellite images, wind data, and notices from Colima Towers and the Mexico City MWO, the Washington VAAC reported that during 4-7 and 9 November ash plumes from Colima rose to altitudes of 4.9-6 km (16,000-20,000 ft) a.s.l. and drifted 13-24 km N, NW, W, SW, and S. On 10 November emissions released about every two hours rose to an altitude of 5.7 (19,000 ft) a.s.l. and drifted SW and WSW.

Geologic Background. The Colima volcanic complex is the most prominent volcanic center of the western Mexican Volcanic Belt. It consists of two southward-younging volcanoes, Nevado de Colima (the 4320 m high point of the complex) on the north and the 3850-m-high historically active Volcán de Colima at the south. A group of cinder cones of late-Pleistocene age is located on the floor of the Colima graben west and east of the Colima complex. Volcán de Colima (also known as Volcán Fuego) is a youthful stratovolcano constructed within a 5-km-wide caldera, breached to the south, that has been the source of large debris avalanches. Major slope failures have occurred repeatedly from both the Nevado and Colima cones, and have produced a thick apron of debris-avalanche deposits on three sides of the complex. Frequent historical eruptions date back to the 16th century. Occasional major explosive eruptions (most recently in 1913) have destroyed the summit and left a deep, steep-sided crater that was slowly refilled and then overtopped by lava dome growth.

Source: Washington Volcanic Ash Advisory Center (VAAC)