Report on Acatenango (Guatemala) — March 1981
Scientific Event Alert Network Bulletin, vol. 6, no. 3 (March 1981)
Managing Editor: Lindsay McClelland.
Acatenango (Guatemala) No visible fumarolic activity; strong sulfur odor near sumit craters
Please cite this report as:
Global Volcanism Program, 1981. Report on Acatenango (Guatemala). In: McClelland, L. (ed.), Scientific Event Alert Network Bulletin, 6:3. Smithsonian Institution. https://doi.org/10.5479/si.GVP.SEAN198103-342080.
14.501°N, 90.876°W; summit elev. 3976 m
All times are local (unless otherwise noted)
Geologists visited the summit 16, 17, and 18 February. There was no visible fumarolic activity around the summit, or in the explosion craters from the volcano's last eruption in 1972. The geologists smelled a strong sulfur odor in the immediate vicinity of the summit craters.
Geologic Background. Acatenango, along with its twin volcano to the south, Volcán Fuego, overlooks the historic former capital city of Antigua, Guatemala. The two principal summits were constructed during three eruptive periods post-dating the roughly 85,000-year-old Los Chocoyos tephra from Atitlán caldera. An ancestral Acatenango volcano collapsed to the south sometime prior to 43,000 years ago, forming La Democracia debris-avalanche deposit, which covers a wide area of the Pacific coastal plain. Construction of Yepocapa, the northern summit of Acatenango, was completed about 20,000 years ago, after which growth of the southern and highest cone, Pico Central (also known as Pico Mayor), began. The first well-documented eruptions took place from 1924 to 1927, although earlier historical eruptions may have occurred. Francisco Vasquez, writing in 1690, noted that in 1661 a volcano that lay aside of Fuego "opened a smoking mouth and still gives off smoke from another three, but without noise."
Information Contacts: T. Bornhorst and C. Chesner, Michigan Tech. Univ.