Report on Colima (Mexico) — 7 January-13 January 2015
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
7 January-13 January 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, 7 January-13 January 2015. Smithsonian Institution and US Geological Survey.
19.514°N, 103.62°W; summit elev. 3850 m
All times are local (unless otherwise noted)
Based on news articles, an explosion from Colima at about 0900 on 3 January generated an ash plume that rose 3 km. Ash fell in the municipalities of Zapotlán El Grande (26 km NE), Gómez Farías (34 km NNE), Concepción de Buenos Aires (63 km NE), Manzanilla de la Paz (72 km NE), Toliman (31 km WNW), Tuxpan (25 km ENE), Zapotiltic (23 km NE), Tamazula de Gordian (42 km NE), Valle de Juárez (85 km NE), Mazamitla (78 km NE), and Tonila (150 km NE). An explosion on 8 January generated an ash plume that rose 2 km and caused ashfall in Tuxpan, Tonila, and Zapotiltic. Another explosion on 11 January generated an ash plume that rose 1 km and caused ashfall in Tuxpan. An ash plume rose 500 m on 12 January and drifted ENE.
Geological Summary. The Colima complex is the most prominent volcanic center of the western Mexican Volcanic Belt. It consists of two southward-younging volcanoes, Nevado de Colima (the high point of the complex) on the north and the historically active Volcán de Colima at the south. A group of late-Pleistocene cinder cones is located on the floor of the Colima graben west and east of the complex. Volcán de Colima (also known as Volcán Fuego) is a youthful stratovolcano constructed within a 5-km-wide scarp, 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, producing thick debris-avalanche deposits on three sides of the complex. Frequent recorded eruptions date back to the 16th century. Occasional major explosive eruptions have destroyed the summit (most recently in 1913) and left a deep, steep-sided crater that was slowly refilled and then overtopped by lava dome growth.