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Volcán Atitlán

Atitlan

Stratovolkan · Guatemala · 3535 m

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. · Foto: Photo by Bill Rose, 1980 (Michigan Technological University). · Wikimedia Commons
Tipe
Stratovolkan
Negara
Guatemala
Wilayah
Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
Ketinggian
3535 m
Koordinat
14.583, -91.186
Letusan terakhir
1853
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
Andesite / Basaltic Andesite
Ringkasan geologi

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.

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
1020 BCE~828 BCE · 1 letusan · VEI maks. ?1281~1473 · 1 letusan · VEI maks. 31473~1664 · 3 letusan · VEI maks. 31664~1856 · 10 letusan · VEI maks. 31020 BCE253 BCE32210891664

Garis waktu rinci

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

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.