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Quaternary volcanoes

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Huaynaputina
Huaynaputina ( ; ) is a volcano in a volcanic high plateau in southern Peru. Lying in the Central Volcanic Zone of the Andes, it was formed by the subduction of the oceanic Nazca Plate under the continental South American Plate. Huaynaputina is a large volcanic crater, which lacks an identifiable mountain profile, with an outer stratovolcano and three younger volcanic vents within an amphitheatre-shaped structure that is either a former caldera or a remnant of glacial erosion. The volcano has erupted dacitic magma.
Chachani
Chachani is a volcanic group in southern Peru, northwest of the city of Arequipa. Part of the Central Volcanic Zone of the Andes, it is above sea level. It consists of several lava domes and individual volcanoes such as Nocarane, along with lava shields such as the Airport Domes. Underneath Chachani lies a caldera.
Viedma
subglacial volcano
Doña Juana
stratovolcano located within the Doña Juana-Cascabel Volcanic Complex National Natural Park
Mount Samsari
mountain in Georgia
Payun Matru
mountain in Argentina
Mount Price
volcano in British Columbia, Canada
Andagua volcanic field
mountain
Ticsani
Ticsani is a volcano in Peru northeast of Moquegua and consists of two volcanoes ("Old Ticsani" and "Modern Ticsani") that form a complex. "Old Ticsani" is a compound volcano that underwent a large collapse in the past and shed of mass down the Rio Tambo valley. Today an arcuate ridge remains of this edifice. "Modern Ticsani" is a complex of three lava domes which were emplaced during the Holocene. Two large eruptions took place during the Holocene, producing the so-called "Grey Ticsani" and "Brown Ticsani" deposits; the last eruption occurred after the 1600 eruption of neighbouring Huaynaputi
Reclus
volcano located in the Southern Patagonian Ice Field, Chile
Mānana
Mānana Island is an uninhabited islet located off Kaupō Beach, near Makapuu at the eastern end of the island of Oahu in the Hawaiian Islands. In the Hawaiian language, mānana means "buoyant". The islet is commonly referred to as Rabbit Island, because its shape as seen from the nearby Oahu shore looks something like a rabbit's head and because it was once inhabited by introduced rabbits. The rabbit colony was established by John Adams Cummins in the 1880s when he ran the nearby Waimānalo plantation. The rabbits were eradicated about a hundred years later because they were destroying the native
Mount Leyli
mountain in Georgia and Armenia
Cape Purvis
Dobson Dome
mountain in Antarctica
Tennena Cone
mountain in British Columbia, Canada
Kunlun Volcanic Group
Volcanic field in Kunlun Mountains, China
Level Mountain
complex volcano in British Columbia, Canada
Shield Nunatak
Nunatak in Victoria Land, Antarctica
The Thumb
mountain in Stikine Region, British Columbia, Canada