Eruption of Lonquimay
4. Jan. 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.
Aus Wikipedia, CC BY-SA · Artikel lesen
Was die Aufzeichnungen sagen
- Wann
- 4. Jan. 1933
- Art
- Vulkanausbruch
- Koordinaten
- 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.
Aus Wikipedia, CC BY-SA · Artikel lesen
Zeitlich und räumlich in der Nähe
- Ranquil massacreJuli 1934 · Massaker
- Eruption of Descabezado Grande5. Juni 1932 · Vulkanausbruch
- Eruption of Llaima9. Feb. 1937 · Vulkanausbruch
- Chile → Peru (cession)1929 · Gebietsveränderung
- Uncertain eruption of Puntiagudo-Cordon Cenizos1930 · Vulkanausbruch
- Eruption of Mocho-Choshuenco16. Juni 1937 · Vulkanausbruch
- Eruption of Calbuco6. Jan. 1929 · Vulkanausbruch
- Earthquake — Chile: Talca, Chillan, Santiago, San Fernando1. Dez. 1928 · Erdbeben · Magnitude 7.6
Die Quelle
- 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.VOTW5-2025.5.3Quellseite