Report on Popocatepetl (Mexico) — 3 December-9 December 2025
Smithsonian Institution / US Geological Survey
Weekly Volcanic Activity Report, 3 December-9 December 2025
Managing Editor: Sally Sennert.
Please cite this report as:
Global Volcanism Program, 2025. Report on Popocatepetl (Mexico) (Sennert, S, ed.). Weekly Volcanic Activity Report, 3 December-9 December 2025. Smithsonian Institution and US Geological Survey.
Popocatepetl
Mexico
19.023°N, 98.622°W; summit elev. 5393 m
All times are local (unless otherwise noted)
The Centro Nacional de Prevención de Desastres (CENAPRED) reported that eruptive activity continued at Popocatépetl during 2-9 December. The seismic network recorded 3-70 long-period events per day, accompanied by steam-and-gas emissions with occasional minor ash content that drifted in various directions. In addition, the seismic network recorded 96 minutes of low-amplitude tremor during 7-8 December and 201 minutes of low-amplitude tremor consisting of 78 minutes of high-frequency tremor and 123 minutes of harmonic tremor during 8-9 December. According to the Washington Volcanic Ash Advisory Center (VAAC) ash plumes visible in webcam and satellite images on 3, 5, 7, and 9 December rose 5.6-6.1 km (18,500-20,000 ft) a.s.l. (about 400 m above the crater rim) and drifted in multiple directions. The Alert Level remained at Yellow, Phase Two (the middle level on a three-color scale) and the public was warned to stay 12 km away from the crater.
Geological Summary. Volcán Popocatépetl, whose name is the Aztec word for smoking mountain, rises 70 km SE of Mexico City to form North America's 2nd-highest volcano. The glacier-clad stratovolcano contains a steep-walled, 400 x 600 m wide crater. The generally symmetrical volcano is modified by the sharp-peaked Ventorrillo on the NW, a remnant of an earlier volcano. At least three previous major cones were destroyed by gravitational failure during the Pleistocene, producing massive debris-avalanche deposits covering broad areas to the south. The modern volcano was constructed south of the late-Pleistocene to Holocene El Fraile cone. Three major Plinian eruptions, the most recent of which took place about 800 CE, have occurred since the mid-Holocene, accompanied by pyroclastic flows and voluminous lahars that swept basins below the volcano. Frequent historical eruptions, first recorded in Aztec codices, have occurred since Pre-Columbian time.
Sources: Centro Nacional de Prevencion de Desastres (CENAPRED), Washington Volcanic Ash Advisory Center (VAAC)
