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Volcán Atitlán

Atitlan

성층화산 · 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. · 사진: Photo by Bill Rose, 1980 (Michigan Technological University). · Wikimedia Commons
화산 유형
성층화산
국가
Guatemala
지역
Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
해발
3535m
좌표
14.583, -91.186
마지막 분화
1853년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Composite
주요 암석
Andesite / Basaltic Andesite
지질학적 요약

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.

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
1020 BCE~828 BCE · 1건 · 최고 VEI ?1281~1473 · 1건 · 최고 VEI 31473~1664 · 3건 · 최고 VEI 31664~1856 · 10건 · 최고 VEI 31020 BCE253 BCE32210891664

상세 타임라인

  1. 1856년VEI 2지질학적 추정
    1856 ~ 진행 중
  2. 1853년VEI 3관측 기록
    1853-05-03 ~ 진행 중
  3. 1852년VEI 2지질학적 추정
    1852 ~ 진행 중
  4. 1843년VEI 2관측 기록
    1843-07 ~ 진행 중
  5. 1837년VEI 2관측 기록
    1837-06 ~ 진행 중
  6. 1833년VEI 2관측 기록
    1833 ~ 진행 중
  7. 1827년VEI 2관측 기록
    1827-03-27 ~ 진행 중
  8. 1827년VEI 3관측 기록
    1827-09-01 ~ 1828-01
  9. 1826년VEI 2관측 기록
    1826-11 ~ 진행 중
  10. 1717년VEI ?지질학적 추정
    1717-08-29 ~ 1721
    Volcano Uncertain
  11. 1663년VEI 2관측 기록
    1663 ~ 진행 중
  12. 1579년VEI 2관측 기록
    1579 ~ 1581-12-31
  13. 1505년VEI 3관측 기록
    1505 ~ 진행 중
  14. 1469년VEI 3관측 기록
    1469 ~ 진행 중
  15. 기원전 1020년 (±150년)VEI ?지질학적 추정
    BCE 1020 ~ 진행 중

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