Report on Colima (Mexico) — 1 June-7 June 2005
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
1 June-7 June 2005
Managing Editor: Gari Mayberry
Please cite this report as:
Global Volcanism Program, 2005. Report on Colima (Mexico). In: Mayberry, G (ed.), Weekly Volcanic Activity Report, 1 June-7 June 2005. Smithsonian Institution and US Geological Survey.
19.514°N, 103.62°W; summit elev. 3850 m
All times are local (unless otherwise noted)
Several explosions occurred at Colima during 1-7 June. On 1 June at 2350 and on 2 June at 0022 explosions produced plumes to heights of ~6.1 km (20,000 ft) a.s.l. The plumes drifted SSW, depositing ash in the towns of Colima and Villa de Alvarez. A large explosion on 5 June at 1420 produced pyroclastic flows, and generated an ash cloud to a height of ~8.9 km (29,200 ft) a.s.l. According to news reports, on 7 June officials in nearby Jalisco state announced a voluntary evacuation of the three villages nearest to the crater, and people in nearby towns were warned to be prepared to evacuate.
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.