Report on Colima (Mexico) — 9 March-15 March 2005
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 9 March-15 March 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, 9 March-15 March 2005. Smithsonian Institution and US Geological Survey.
19.514°N, 103.62°W; summit elev. 3850 m
All times are local (unless otherwise noted)
An eruption at Colima on 10 March at 0810 produced pyroclastic flows that traveled up to 3 km down the volcano's flanks in all directions. In addition, an E-drifting ash cloud was generated that rose to a height of ~2 km above the crater. Ash fell in and near the cities of Guzmán and Jalisco. On 13 March at 1528 a large explosion produced a pyroclastic flow down several ravines: El Muerto, Montegrande, San Antonio, and the eastern part of El Cordobán. According to the Mexico City MWO, an ash plume rose to ~5 km above the crater. Ash and rock fragments fell in the towns of Mazos and Jalisco, ~12.5 km NE of the volcano.
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 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 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, producing thick debris-avalanche deposits on three sides of the complex. Frequent historical 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.