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Volcán Atitlán

Atitlan

Stratovolcano · Guatemala · 3535m

Volcán Atitlán directly overlies the inferred margin of the Pleistocene Atitlán III caldera, whose northern rim lies across Lake Atitlán. The Atitlán stratovolcano is adjacent to Tolimán to its north (seen just to the right of Atitlán's summit). The historically active Atitlán is younger than Tolimán, although their earlier activity overlapped. Atitlán’s surface is composed of tephra, reflecting its predominantly explosive eruptions that have been recorded since the 15th century.
Volcán Atitlán directly overlies the inferred margin of the Pleistocene Atitlán III caldera, whose northern rim lies across Lake Atitlán. The Atitlán stratovolcano is adjacent to Tolimán to its north (seen just to the right of Atitlán's summit). The historically active Atitlán is younger than Tolimán, although their earlier activity overlapped. Atitlán’s surface is composed of tephra, reflecting its predominantly explosive eruptions that have been recorded since the 15th century. · Photo: Photo by Bill Rose, 1980 (Michigan Technological University). · Wikimedia Commons
Type
Stratovolcano
Country
Guatemala
Region
Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
Elevation
3535m
Coordinates
14.583, -91.186
Last eruption
1853
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Landform
Composite
Major rock type
Andesite / Basaltic Andesite
Geological summary

Volcán Atitlán is one of several conical stratovolcanoes in the Guatemalan highlands. Along with Tolimán to the north, it forms a dramatic backdrop to Lake Atitlán. The summit directly overlies the inferred margin of the Pleistocene Atitlán III caldera and is the highest of three large post-caldera stratovolcanoes constructed near the southern caldera rim. The volcano consequently post-dates the eruption of the voluminous, roughly 85,000-year-old rhyolitic Los Chocoyos tephra associated with formation of the Atitlán III caldera. The andesitic Volcán Atitlán is younger than Tolimán 3 km away on the N flank, although their earlier activity overlapped. In contrast to Tolimán, Atitlán displays a thick pyroclastic cover. The northern side of the volcano is wooded to near the summit, whereas the upper 1,000 m of the southern slopes are unvegetated. Predominantly explosive eruptions have been recorded since the 15th century.

Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
1020 BCE~828 BCE · 1 eruptions · max VEI ?1281~1473 · 1 eruptions · max VEI 31473~1664 · 3 eruptions · max VEI 31664~1856 · 10 eruptions · max VEI 31020 BCE253 BCE32210891664

Detailed timeline

  1. 1856VEI 2Geological estimate
    1856 – Ongoing
  2. 1853VEI 3Observed
    1853-05-03 – Ongoing
  3. 1852VEI 2Geological estimate
    1852 – Ongoing
  4. 1843VEI 2Observed
    1843-07 – Ongoing
  5. 1837VEI 2Observed
    1837-06 – Ongoing
  6. 1833VEI 2Observed
    1833 – Ongoing
  7. 1827VEI 2Observed
    1827-03-27 – Ongoing
  8. 1827VEI 3Observed
    1827-09-01 – 1828-01
  9. 1826VEI 2Observed
    1826-11 – Ongoing
  10. 1717VEI ?Geological estimate
    1717-08-29 – 1721
    Volcano Uncertain
  11. 1663VEI 2Observed
    1663 – Ongoing
  12. 1579VEI 2Observed
    1579 – 1581-12-31
  13. 1505VEI 3Observed
    1505 – Ongoing
  14. 1469VEI 3Observed
    1469 – Ongoing
  15. 1020 BCE (±150 yrs)VEI ?Geological estimate
    BCE 1020 – Ongoing

External links

⚠ For reference only. Not for emergency response.