Pico de Orizaba Volcano

Pico de Orizaba volcano (Volcán Citlaltépetl) is a large active stratovolcano, Mexico's highest mountain and the highest volcano of North America. It is located at the southern end of Citlaltépetl–Cofre de Perote Volcanic Range, and the only volcano in this area with historic activity.
Historical eruptions have consisted of moderate explosive activity and the effusion of dacitic lava flows. The latest eruption of the volcano were in 1545, 1566, 1630 and 1687.
Pico de Orizaba volcano eruptions: 1157(?), 1175, 1187(?), 1260, 1351(?), 1533-39(?), 1545-55, 1566, 1569-89, 1613, 1687, 1846
Latest nearby earthquakes
Date and Time | Mag / Depth | Distance / Location | |||
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Apr 26, 01:31 pm (GMT -6) | 1.8 4 km | 8.4 km (5.2 mi) to the N | ![]() | Info | |
Wednesday, April 23, 2025 GMT (1 quake) | |||||
Apr 23, 03:24 am (Mexico City) | 2.5 6.8 km | 4.7 km (2.9 mi) to the N | ![]() | Info | |
Tuesday, April 22, 2025 GMT (2 quakes) | |||||
Apr 21, 06:55 pm (Mexico City) | 3? 5.1 km | 24 km (15 mi) to the NW | ![]() | Info | |
Apr 21, 06:48 pm (Mexico City) | 2? 5.2 km | 5.1 km (3.2 mi) to the W | ![]() | Info |
Background
Pico de Orizaba volcano was formed in 3 stages beginning during the mid-Pleistocene. Orizaba lies at the southern end of a volcanic chain extending north to Cofre de Perote volcano and towers up to 4400 m above its eastern base. Construction of the initial Torrecillas and Espolón de Oro volcanoes was contemporaneous with growth of Sierra Negra volcano on the SW flank and was followed by edifice collapses that produced voluminous debris avalanches and lahars. The modern Citlaltépetl volcano was constructed during the late Pleistocene and Holocene of viscous andesitic and dacitic lavas, forming the current steep-sided cone. Repetitive explosive eruptions beginning during the early Holocene accompanied lava dome growth and lava effusion.Pico de Orizaba Volcano Photos

Significant volcanic eruptions: Pico de Orizaba volcano
Additionally, there are 4 uncertain or discredited eruptions from Pico de Orizaba volcano.
Date | Note | VEI | Deaths | Damage | |
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Historical obs./docs. | 2 | ||||
Historical obs./docs. | 2 | ||||
Historical obs./docs. | 0 | ||||
Historical obs./docs. | 2 | ||||
Historical obs./docs. | 2 | ||||
Historical obs./docs. | 2 | ||||
?? | Uncertain Eruption | 2? | |||
?? | Uncertain Eruption | 2 | |||
3 | |||||
?? | Uncertain Eruption | 2 | |||
3? | |||||
?? | Uncertain Eruption | 2 | |||
3 | |||||
3 | |||||
3 | |||||
3 | |||||
3 | |||||
3 | |||||
3 | |||||
4 | |||||
3 | |||||
3 |
Pico de Orizaba Volcano FAQ
+When was the last eruption of Pico de Orizaba volcano?
The last confirmed eruption of Pico de Orizaba occurred in 1846.
+How often does Pico de Orizaba volcano erupt?
Since 1545 AD, Pico de Orizaba volcano has had at least 6 historically documented eruptions. This means that it erupts on average every 80 years.
Many eruptions of Pico de Orizaba have lasted more than one year. In total, the volcano has been in eruption during 36 out of 480 years until now. In other words, Pico de Orizaba has been active at least one in 13.3 years on average. Note that this value is likely an underestimate, because the known history of eruptions from Pico de Orizaba is likely incomplete, especially further back in time.
+When was the largest eruption of Pico de Orizaba volcano?
The largest eruption known from the younger geological history of Pico de Orizaba volcano occurred around 6710 BC. It ranks as a strombolian to vulcanian eruption with a magnitude 2 on the VEI (Volcanic Explosivity Index) scale.
Latest satellite images
Pico de Orizaba Volcano Maps





















