火山噴火

Eruption of Lonquimay

1887年6月2日 – 1890年1月 · 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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時期
1887年6月2日 – 1890年1月
種類
火山噴火
座標
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.

出典: Wikipedia、CC BY-SA · 記事を読む

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