ثوران بركاني

Eruption of Cerro Hudson

790 ق.م · 45.90° S, 72.97° W

Hudson Volcano is the most active volcano in the southern part of the Southern Volcanic Zone of the Andes Mountains in Chile, having erupted most recently in 2011. It was formed by the subduction of the oceanic Nazca Plate under the continental South American Plate.

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متى
790 ق.م
النوع
ثوران بركاني
إحداثيات
45.90° S, 72.97° W
Date uncertainty
± 75 years
Unit
Tephra layer HW6
Dated by
Isotopic: 14C (calibrated)
Volcano number
358057
Eruption number
12292

Hudson Volcano

Mountain in Chile

Hudson Volcano is the most active volcano in the southern part of the Southern Volcanic Zone of the Andes Mountains in Chile, having erupted most recently in 2011. It was formed by the subduction of the oceanic Nazca Plate under the continental South American Plate. South of Hudson is a smaller volcano, followed by a long gap without active volcanoes, then the Austral Volcanic Zone.

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