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Nevado de Longaví   »  Summary

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Nevado de Longaví

Nevado de Longaví Photo

Country:Chile
Subregion Name:Central Chile
Volcano Number:1507-063
Volcano Type: Stratovolcano
Volcano Status:Radiocarbon
Last Known Eruption: 4890 BC ± 75 years
Summit Elevation: 3242 m 10,636 feet
Latitude: 36.193°S 36°11'35"S
Longitude: 71.161°W 71°9'39"W

The conical, glacier-clad Nevado de Longaví volcano is a late-Pleistocene to Holocene, dominantly andesitic stratovolcano constructed over a basement of Tertiary volcaniclastic and granitic rocks. Two edifice-collapse events modified the eastern and SW flank of a pre-Holocene volcano, and Holocene activity has been concentrated at the summit region and on the eastern flanks of the volcano. Andesitic-to-dacitic lava domes occupy the summit region, and a Holocene dome forms the 3242-m-high summit of Longaví. The last eruptions produced a lava dome in the upper part of the collapse scarp and summit region that partially collapsed to the east, forming block-and-ash flow deposits. No historical eruptions are known, although fumarolic activity continues.

Global Volcanism ProgramDepartment of Mineral SciencesNational Museum of Natural HistorySmithsonian Institution

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