El Chichón
Mexico's Deadliest Modern Eruption
1,150 m
1982
Lava dome(s)
Mexico
Location
Loading map...
Volcanic Hazards & Risk Assessment
Primary Hazards
- Lava flows and fountaining
- Volcanic gas emissions
- Local explosive activity
Risk Level
Geological Composition & Structure
Rock Types
Tectonic Setting
Age & Formation
Eruption Statistics & Analysis
| Metric | Value | Global Ranking | Significance |
|---|---|---|---|
| Total Recorded Eruptions | Unknown | Low | Moderately active volcano |
| Maximum VEI | VEI Unknown | Minor | Local impact potential |
| Recent Activity | 44 years ago | Recent | Recently active |
Monitoring & Alert Status
Monitoring Networks
Current Status
Authority Sources
Other Volcanoes in Mexico
- Volcán de Colima
Stratovolcano
- Michoacán-Guanajuato Volcanic Field
Volcanic field
- Pico de Orizaba
Stratovolcano
- Popocatépetl
Stratovolcano
Interesting Facts
El Chichón's 1982 eruption injected 7–10 megatons of SO₂ into the stratosphere — more than any eruption since Krakatau in 1883 — despite being a relatively modest VEI 5 event.
The 1982 eruption killed approximately 2,000 people, making it the deadliest volcanic event in Mexican history in the modern era.
Global temperatures decreased by approximately 0.3–0.5°C in the 1–2 years following the eruption due to stratospheric sulfuric acid aerosols.
Before 1982, El Chichón was so poorly known that it did not appear on most Mexican volcanic hazard maps despite being capable of VEI 5 eruptions.
The eruption destroyed nine Zoque indigenous villages and virtually the entire population of Francisco León, a village of approximately 1,000 people at the volcano's base.
Four VEI 5 eruptions in the past ~4,000 years give El Chichón one of the highest ratios of large eruptions to total eruptions of any volcano on Earth.
The crater lake formed after 1982 has a pH as low as 1.7 — roughly as acidic as stomach acid — and temperatures reaching 52°C.
El Chichón's magma contains abundant anhydrite (calcium sulfate), a mineral rarely found in volcanic rocks, which explains its exceptional sulfur output.
The 1982 eruption's global cooling effect demonstrated that volcanic sulfur content, not just eruption volume, determines a volcano's climate impact.
The Chiapanecan Volcanic Arc, where El Chichón sits, is separated from Mexico's main Transmexican Volcanic Belt by over 300 km.
The 1982 disaster contributed directly to the establishment of Mexico's Centro Nacional de Prevención de Desastres (CENAPRED) in 1988.
The ~780 CE eruption of El Chichón has been proposed as a potential factor in disruptions to Classic Maya civilization, though the link remains debated.