Report on Colima (Mexico) — 29 May-4 June 2019
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 29 May-4 June 2019
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2019. Report on Colima (Mexico). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 29 May-4 June 2019. Smithsonian Institution and US Geological Survey.
19.514°N, 103.62°W; summit elev. 3850 m
All times are local (unless otherwise noted)
Centro Universitario de Estudios e Investigaciones de Vulcanologia - Universidad de Colima reported that during 25-31 May small explosions and intermittent steam-and-gas emissions mainly from the NE side of the crater continued to be recorded. During overflights conducted during 23-24 May scientists observed that the new feature (a crack or cavity) reported the previous week had become a hole due to the combination of excavation due to explosions and probable subsidence. The maximum temperature recorded with a portable thermal camera was 252 degrees Celsius, an increase of 80 degrees since recorded on 1 May.
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.