New Updates On POPOCATÉPETL And MEXICO—Crater GLOWING As 30 Million Watch CENAPRED Yellow Phase 2

Popocatépetl — the Smoking Mountain — is one of Mexico's most closely monitored volcanoes, located between Puebla, Morelos and Estado de México, approximately 55 km east of Mexico City and 45 km west of Puebla. More than 30 million people live within 80 km of the summit. The volcano has been in continuous eruptive activity since December 21, 1994, when it reawakened after roughly 70 years of dormancy. Since 2003, CENAPRED — the Centro Nacional de Prevención de Desastres — has classified the volcano under Yellow Phase 2 of the national Volcanic Alert Traffic Light system. Between June 2 and June 5, 2026, the volcano produced a notable cluster of activity that drew renewed national attention. On the evening of June 2, cameras captured Popocatépetl expelling incandescent material from its crater while an electrical storm developed around the summit. Protection Civil issued an ash dispersion warning for parts of Puebla, Estado de México and Morelos, depending on wind direction. On June 3, CENAPRED's daily bulletin reported 48 exhalations, 280 minutes of exhalation sequences, 426 minutes of tremor — more than seven hours of internal seismic energy in a single 24-hour cycle — one explosion, and one volcanotectonic earthquake. On June 5, CENAPRED reported 108 exhalations accompanied by water vapor, volcanic gases and ash. The Volcanic Alert Traffic Light remains at Yellow Phase 2. The alert has not been raised. Yellow Phase 2 does not mean a catastrophic eruption is imminent. Yellow Phase 2 means the volcano is active and can produce exhalations, ash emissions, explosions, incandescent fragments and lahars in ravines during heavy rain. The central editorial question of this forecast is not whether Popocatépetl is awake — it has been awake for 32 years — but whether the visible glow of June 2, the long tremor episode of June 3, and the 108 exhalations of June 5 are part of the established Yellow Phase 2 pattern, or the beginning of a stronger phase building under central Mexico. Popocatépetl is a stratovolcano sitting on the Trans-Mexican Volcanic Belt, where the Cocos plate subducts under the North American plate at approximately 7 cm per year. The magma is andesite-dacite — high-viscosity, gas-rich, slow to flow, quick to fragment — and reaches temperatures of approximately 900°C (1,650°F) inside the eruptive column. Historical context: between 2,000 and 1,800 years ago, a village known as Tetimpa lived on the northeast flank of Popocatépetl, in what is now the state of Puebla. The settlement of approximately 3,000 to 4,000 people, with more than 600 wattle-and-daub houses built on stone talud-tablero platforms and small clay effigies of the volcano placed inside household shrines, was destroyed in the first century AD by ash and pumice airfall. Mexican archaeologists from Universidad de las Américas Cholula have been excavating the site since 1993 and call it the "Little Pompeii of Mexico." A second eruption between AD 700 and 900 destroyed the re-settled population. The northeast flank that the volcano buried two millennia ago is the same direction Protection Civil is warning about this week — Puebla, Estado de México, Morelos. CENAPRED has not declared a new phase, has not announced an end to the recent activity, and has not raised the alert level. Independent monitoring of seismic, gas and thermal data continues at the volcano in coordination with the Instituto de Geofísica UNAM. The question for the residents of San Pedro Nexapa, Atlixco, Cholula, Tlamanalco and the broader Puebla-Mexico City corridor is whether the recent four-day cluster is another pulse the system can absorb, or a signal that pressure beneath central Mexico is building again.

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