火山噴火

Eruption of Lonquimay

1933年1月4日 · 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.

出典: Wikipedia、CC BY-SA · 記事を読む

1933 を地図で見るWikipedia
1933 を地図で見る

記録が伝えること

時期
1933年1月4日
種類
火山噴火
座標
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.

出典: Wikipedia、CC BY-SA · 記事を読む

時期と場所が近い出来事

情報源