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Report on Popocatepetl (Mexico) — 11 January-17 January 2012


Popocatepetl

Smithsonian Institution / US Geological Survey
Weekly Volcanic Activity Report, 11 January-17 January 2012
Managing Editor: Sally Sennert.

Please cite this report as:

Global Volcanism Program, 2012. Report on Popocatepetl (Mexico) (Sennert, S, ed.). Weekly Volcanic Activity Report, 11 January-17 January 2012. Smithsonian Institution and US Geological Survey.

Weekly Report (11 January-17 January 2012)

Popocatepetl

Mexico

19.023°N, 98.622°W; summit elev. 5393 m

All times are local (unless otherwise noted)


CENAPRED reported that during 11-17 January steam-and-gas emissions rose from Popocatépetl; the plumes contained small amounts of ash during 13-17 January. Crater incandescence was observed at night during 16-17 January.

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.

Source: Centro Nacional de Prevencion de Desastres (CENAPRED)