Eruption of Lonquimay
2 juin 1887 – janv. 1890 · 38.38° S, 71.59° W
Lonquimay Volcano is a stratovolcano of late-Pleistocene to dominantly Holocene age, with the shape of a truncated cone. The cone is largely andesitic, though basaltic and dacitic rocks are present. It is located in the La Araucanía Region of Chile, immediately SE of Tolhuaca volcano.
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Ce que disent les sources
- Quand
- 2 juin 1887 – janv. 1890
- Type
- Éruption volcanique
- Coordonnées
- 38.38° S, 71.59° W
- Vei
- 3
- Vent
- NE flank
- Dated by
- Observations: Reported
- Volcano number
- 357100
- Eruption number
- 12013
Lonquimay (volcano)
Mountain in Chile
Lonquimay Volcano is a stratovolcano of late-Pleistocene to dominantly Holocene age, with the shape of a truncated cone. The cone is largely andesitic, though basaltic and dacitic rocks are present. It is located in the La Araucanía Region of Chile, immediately SE of Tolhuaca volcano. Sierra Nevada and Llaima are their neighbors to the south.
Source : Wikipedia, CC BY-SA · Lire l’article
Proches dans le temps et dans l’espace
La source
- Smithsonian GVP Volcanoes of the World: Holocene eruptionsGlobal Volcanism Program, Smithsonian InstitutionSmithsonian terms of use: personal, educational and non-commercial use, with creditGlobal Volcanism Program, Smithsonian Institution: Volcanoes of the World v5.3, https://doi.org/10.5479/si.GVP.VOTW5-2025.5.3Page source