Logo link to homepage

Report on Colima (Mexico) — 12 May-18 May 2004

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 12 May-18 May 2004
Managing Editor: Gari Mayberry

Please cite this report as:

Global Volcanism Program, 2004. Report on Colima (Mexico). In: Mayberry, G (ed.), Weekly Volcanic Activity Report, 12 May-18 May 2004. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (12 May-18 May 2004)


Colima

Mexico

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

All times are local (unless otherwise noted)


Universidad de Colima reported on 15 May that low-intensity activity continued at Colima, with an average of three ash-containing explosions daily during the previous few days. The plumes rose to less than 2 km above the volcano and drifted W, N, and E. Some explosions produced pyroclastic flows to distances less than 2 km. On 14 May at 1028 an explosion produced a plume to ~2 km above the volcano that drifted E. In addition, three small pyroclastic flows traveled down the volcano's W, N, and E flanks.

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.

Sources: Centro Universitario de Estudios e Investigaciones de Vulcanologia - Universidad de Colima, Washington Volcanic Ash Advisory Center (VAAC)