Report on Colima (Mexico) — 8 November-14 November 2000
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 8 November-14 November 2000
Managing Editor: Gari Mayberry
Please cite this report as:
Global Volcanism Program, 2000. Report on Colima (Mexico). In: Mayberry, G (ed.), Weekly Volcanic Activity Report, 8 November-14 November 2000. Smithsonian Institution and US Geological Survey.
19.514°N, 103.62°W; summit elev. 3850 m
All times are local (unless otherwise noted)
The Volcanological Observatory of Colima University reported that small exhalations occurred at Colima at 1250 on 8 November, 1327 on 9 November, and at 1728 on 10 November. The Mexico City MWO reported that the 10 November exhalation produced an ash cloud that rose to 6 km a.s.l. and was blown to the ENE. The Washington VAAC reported that the ash cloud was not visible in GOES-8 imagery. According to the observatory, the events did not exceed the established safety limits so the zone of exclusion remained at 6.5 km around 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 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.