Mexico · Stratovolcano
Citlaltepetl
Orizaba, Pico de
- Type
- Stratovolcano
- Elevation
- 5564m
- Last eruption
- 1846

- Type
- Stratovolcano
- Country
- Mexico
- Region
- Middle America & Caribbean / Trans-Mexican Volcanic Arc
- Elevation
- 5564m
- Coordinates
- 19.030, -97.270
- Last eruption
- 1846
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic andesite
Geological summary
Pico de Orizaba (Volcán Citlaltépetl), México's highest peak and North America's highest volcano, lies at the southern end of a volcanic chain extending north to Cofre de Perote volcano, east of the Serdan-Oriental Basin. The edifice was formed in three stages beginning during the mid-Pleistocene. 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 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. Recorded eruptions have consisted of moderate explosive activity and the effusion of dacitic lava flows. The last known observations of activity were in 1846 CE.
From Wikipedia
Citlaltépetl, otherwise known as Pico de Orizaba, is an active volcano and the highest volcano in North America, as well as the highest mountain in Mexico and third highest peak in North America, after Denali of the United States and Mount Logan of Canada. It rises 5,636 metres (18,491 ft) above sea level in the eastern end of the Trans-Mexican Volcanic Belt, on the border between the states of Veracruz and Puebla. The volcano is currently dormant but not extinct, with the last eruption taking place during the 19th century. It is the second most prominent volcanic peak in the world after Mount Kilimanjaro. Pico de Orizaba is ranked 16th by topographic isolation.
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Eruption history
27 recordedGlossaryDetailed timeline
- 1846VEI 2Observed1846-07-02 – end unknown
- 1687VEI 2Observed1687 – end unknown
- 1613VEI 0Observed1613 – end unknown
- 1569VEI 2Observed1569 – 1589
- 1566VEI 2Observed1566 – end unknown
- 1545VEI 2Observed1545 – 1555
- 1533VEI 2Method not stated1533 – 1539
- 1351VEI 2Method not stated1351 – end unknown
- 1260 (±50 yrs)VEI 3Geological estimate1260 – end unknown
- 1187VEI 2Method not stated1187 – end unknown
- 1175VEI 3Geological estimate1175 – end unknown
- 1157VEI 2Method not stated1157 – end unknown
- 220 (±75 yrs)VEI 3Geological estimate220 – end unknown
- 140 (±50 yrs)VEI 3Geological estimate140 – end unknown
- 90 (±40 yrs)VEI 3Geological estimate90 – end unknown
- 40 (±40 yrs)VEI 3Geological estimate40 – end unknown
- 780 BCE (±60 yrs)VEI 3Geological estimate780 BCE – end unknown
- 1500 BCE (±75 yrs)VEI 3Geological estimate1500 BCE – end unknown
- 2110 BCE (±100 yrs)VEI 3Geological estimate2110 BCE – end unknown
- 2300 BCE (±75 yrs)VEI 4Geological estimate2300 BCE – end unknown
- 2500 BCE (±75 yrs)VEI 3Geological estimate2500 BCE – end unknown
- 2780 BCE (±75 yrs)VEI 3Geological estimate2780 BCE – end unknown
- 4690 BCE (±300 yrs)VEI 3Geological estimate4690 BCE – end unknown
- 6220 BCE (±75 yrs)VEI 3Geological estimate6220 BCE – end unknown
- 6710 BCE (±150 yrs)VEI 5Geological estimate6710 BCE – end unknown
- 7030 BCE (±50 yrs)VEI 4Geological estimate7030 BCE – end unknown
- 7530 BCE (±40 yrs)VEI ?Geological estimate7530 BCE – end unknown
Nearby volcanoes
External links
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