Volcán San José on the far left horizon rises to the north above ice pinnacles at the Nieves Negras pass on the Chile/Argentina border.
The summit (5856 m) of San José is formed by a cluster of six Holocene craters, pyroclastic cones, and blocky lava flows that lie within a series of elongated, 0.5 x 2 km wide nested craters.
The summit (5856 m) of San José is formed by a cluster of six Holocene craters, pyroclastic cones, and blocky lava flows that lie within a series of elongated, 0.5 x 2 km wide nested craters.
Mild phreatomagmatic eruptions were recorded at San José in the 19th and 20th centuries.
Its last eruption was in 1960.
Photo courtesy of Oscar González-Ferrán (University of Chile)
Fair use of copyrighted material is permitted by Smithsonian.
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Il vulcano San José, situato alla frontiera tra Cile e Argentina, possiede una sommità formata da 6 crateri dell'Olocene, da coni piroclastici e da colate di lava solidificata. Il rilievo culmina a 5856 m.
Photo courtesy of Oscar González-Ferrán (University of Chile)
Fair use of copyrighted material is permitted by Smithsonian.
http://www.si.edu/copyright/
Il vulcano San José, situato alla frontiera tra Cile e Argentina, possiede una sommità formata da 6 crateri dell'Olocene, da coni piroclastici e da colate di lava solidificata. Il rilievo culmina a 5856 m.
Le ultime eruzioni freatomagmatiche risalgono all'800 e 900.
La sua ultima risale al 1960.
Le volcan San José, situé à la frontière entre le Chilie et l'Argentine, possède un sommet formé par 6 cratères appartenant à l'holocène, des cones pyroclastiques et des coulées de lave solidifiée. Le relief culmine à 5856 m.
Ses dernières éruptions phréatomagmatiques remontent aux XIXe et XX.
Sa dernière éruption a eu lieu en 1960.
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