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Iztaccihuatl

Stratovolcano in Mexico

Key Facts

Elevation

5,230 m (17,159 ft)

Type

Stratovolcano

Location

19.179°, -98.642°

Region

Trans-Mexican Volcanic Arc

Rock Type

Andesite / Basaltic Andesite

Tectonic Setting

Subduction zone

Location

Loading map...

Overview

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.

Volcanic Hazards & Risk Assessment

Primary Hazards

  • Pyroclastic flows
  • Lava flows
  • Volcanic bombs and ballistics
  • Lahars and mudflows

Risk Level

Population at RiskModerate
Infrastructure RiskModerate
Aviation RiskSignificant

Geological Composition & Structure

Rock Types

Primary
Andesite / Basaltic Andesite
Silica Content
Intermediate (57-63% SiO₂)

Tectonic Setting

Subduction zone
Formed by oceanic plate subduction, typically producing explosive eruptions due to water-rich magmas.

Age & Formation

Epoch
Holocene
Evidence
Evidence Credible

Eruption Statistics & Analysis

MetricValueGlobal RankingSignificance
Total Recorded EruptionsUnknownLowModerately active volcano
Maximum VEIVEI UnknownMinorLocal impact potential
Recent ActivityUnknownHistoricalHistorically active

Monitoring & Alert Status

Monitoring Networks

Global Volcanism Program
International eruption database

Current Status

Normal
No recent activity. Routine monitoring continues.

Nearby Volcanoes in Middle America-Caribbean Volcanic Regions

Regional Volcanic Activity
The Middle America-Caribbean Volcanic Regions contains multiple active volcanic systems. Cross-regional magma interactions and tectonic stresses can influence eruption patterns across the entire arc. Monitor regional seismic activity and volcanic alerts.

Quick Info

  • Smithsonian ID: 341082
  • Evidence: Evidence Credible
  • Epoch: Holocene

About the Photo

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 by José Macías, 1995 (Universidad Nacional Autónoma de México).

Basic Information

This page shows basic data from the Smithsonian Global Volcanism Program. For more detailed information, visit the official Smithsonian page.