Извержение вулкана

Eruption of Lonquimay

4 янв. 1933 г. · 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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Что говорят записи

Когда
4 янв. 1933 г.
Вид
Извержение вулкана
Координаты
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.

Источник: Wikipedia, CC BY-SA · Читать статью

Рядом по времени и месту

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