Iztaccihuatl
성층화산 · Mexico · 5230m

- 화산 유형
- 성층화산
- 국가
- Mexico
- 지역
- Middle America-Caribbean Volcanic Regions / Trans-Mexican Volcanic Arc
- 해발
- 5230m
- 좌표
- 19.179, -98.642
- 마지막 분화
- 미확인
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
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.
Wikipedia 요약
영어 요약Iztaccíhuatl 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).
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