Mount Hudson (Spanish: Volcán Hudson, Spanish: Cerro Hudson, Monte Hudson) is a volcano in the rugged mountains of southern Chile. Lying in the Southern Volcanic Zone of the Andes, it was formed by the subduction of the oceanic Nazca Plate under the continental South American Plate. The Nazca Plate ends there at the Chile Triple Junction; south of Hudson is a smaller volcano, followed by a long gap without active volcanoes that separates the Southern Volcanic Zone from the Austral Volcanic Zone. Hudson has the form of a 10-kilometre-wide (6-mile) volcanic caldera filled with ice. The Huemules Glacier emerges from the northwestern side of the caldera. The volcano has erupted rocks ranging from basalt to rhyolite, but large parts of the caldera are formed by non-volcanic rocks.
The volcano erupted numerous times in the late Pleistocene[a] and Holocene[b], forming widespread tephra deposits both in the proximity of Hudson and in the wider region, and is the most active volcano in the region. The last eruption was in 2011.
Four large eruptions took place in 17,300–17,440 BP ("H0 eruption"), 7,750 BP ("H1 eruption"), 4,200 BP ("H2 eruption") and in 1991 AD ("H3 eruption"); the second is among the most intense volcanic eruptions in South America during the Holocene. A smaller eruption occurred in 1971. The 7,750 BP and 1991 eruptions had a substantial impact on the human population of Patagonia and (for the 7,750 BP eruption) Tierra del Fuego: The 7,750 BP eruption devastated the local ecosystem and may have caused substantial shifts in human settlement and lifestyle. During the 1991 eruption, volcanic ash covered a large area in Chile and neighbouring Argentina, causing high mortality in farm animals, aggravating an existing economic crisis, and depositing ash as far as Antarctica.
^GVP 2023, General Information.
^ abICC 2018.
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MountHudson (Spanish: Volcán Hudson, Spanish: Cerro Hudson, Monte Hudson) is a volcano in the rugged mountains of southern Chile. Lying in the Southern...
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Global Information
