Skip to main content

Iztaccihuatl

Stratovolcano · Mexico · 5230m

Iztaccíhuatl is a massive 450 km3 stratovolcano SE of Mexico City, seen here from the SW. The summit is composed of several overlapping edifices, including the northernmost peak, La Cabeza (left), the snow-capped high point El Pecho, and Las Rodillas (below the lower Ayoloco glacier near the center). Most activity ceased during the Pleistocene, and the volcano has been extensively glaciated, as seen by the sharp-crested glacial moraines below the Ayoloco glacier.
Iztaccíhuatl is a massive 450 km3 stratovolcano SE of Mexico City, seen here from the SW. The summit is composed of several overlapping edifices, including the northernmost peak, La Cabeza (left), the snow-capped high point El Pecho, and Las Rodillas (below the lower Ayoloco glacier near the center). Most activity ceased during the Pleistocene, and the volcano has been extensively glaciated, as seen by the sharp-crested glacial moraines below the Ayoloco glacier. · Photo: Photo by José Macías, 1995 (Universidad Nacional Autónoma de México). · Wikimedia Commons
Type
Stratovolcano
Country
Mexico
Region
Middle America-Caribbean Volcanic Regions / Trans-Mexican Volcanic Arc
Elevation
5230m
Coordinates
19.179, -98.642
Last eruption
Unknown
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Landform
Composite
Major rock type
Andesite / Basaltic Andesite
Geological summary

Iztaccíhuatl (the "Woman in White") presents the profile of a sleeping woman as seen from the Valley of Mexico. A series of overlapping cones constructed along a NNW-SSE line to the south of the Pleistocene Llano Grande caldera forms the summit ridge of the massive 450 km3 volcano. Andesitic and dacitic Quaternary volcanism has taken place from vents at or near the summit. Valley headwalls near the summit vent (El Pecho) have lava flows and tuff deposits post-dating a glaciation about 11,000 years ago. The youngest vents are located at the summit and a depression at 5,100 m along the summit ridge midway between El Pecho and Los Pies (White, 1986). Nixon (1989) considered all summit lavas to be Pleistocene, but noted a postglacial dacitic vent on the S flank of Iztaccíhuatl, north of the saddle between it and Popocatépetl.

From Wikipedia

Iztaccíhuatl or Ixtaccíhuatl is a 5,230 m (17,160 ft) dormant volcanic mountain in Mexico located on the border between the State of Mexico and Puebla within Izta-Popo Zoquiapan National Park. It is the nation's third highest, after Pico de Orizaba at 5,636 m (18,491 ft), and Popocatépetl at 5,426 m (17,802 ft).

Wikipedia · CC BY-SA · Read full article

Eruption history

Detailed timeline

No eruption records available.

External links

⚠ For reference only. Not for emergency response.