Eruption of Lonquimay
4 janv. 1933 · 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
- 4 janv. 1933
- Type
- Éruption volcanique
- Coordonnées
- 38.38° S, 71.59° W
- Vei
- 2
- Dated by
- Observations: Reported
- Volcano number
- 357100
- Eruption number
- 12014
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
- Ranquil massacrejuil. 1934 · Massacre
- Eruption of Descabezado Grande5 juin 1932 · Éruption volcanique
- Eruption of Llaima9 févr. 1937 · Éruption volcanique
- Chile → Peru (cession)1929 · Changement territorial
- Uncertain eruption of Puntiagudo-Cordon Cenizos1930 · Éruption volcanique
- Eruption of Mocho-Choshuenco16 juin 1937 · Éruption volcanique
- Eruption of Calbuco6 janv. 1929 · Éruption volcanique
- Earthquake — Chile: Talca, Chillan, Santiago, San Fernando1 déc. 1928 · Séisme · Magnitude 7.6
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