Eruption of Lonquimay
4 de jan. de 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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O que dizem os registros
- Quando
- 4 de jan. de 1933
- Tipo
- Erupção vulcânica
- Coordenadas
- 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.
Da Wikipedia, CC BY-SA · Ler o artigo
Perto no tempo e no espaço
- Ranquil massacrejul. de 1934 · Massacre
- Eruption of Descabezado Grande5 de jun. de 1932 · Erupção vulcânica
- Eruption of Llaima9 de fev. de 1937 · Erupção vulcânica
- Chile → Peru (cession)1929 · Mudança territorial
- Uncertain eruption of Puntiagudo-Cordon Cenizos1930 · Erupção vulcânica
- Eruption of Mocho-Choshuenco16 de jun. de 1937 · Erupção vulcânica
- Eruption of Calbuco6 de jan. de 1929 · Erupção vulcânica
- Earthquake — Chile: Talca, Chillan, Santiago, San Fernando1 de dez. de 1928 · Terremoto · Magnitude 7.6
A fonte
- 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.VOTW5-2025.5.3Página da fonte