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Dacitic lava dome in northern Chile
Chillahuita is a dacitic lava dome in northern Chile. It may have formed after the Pleistocene, although argon-argon dating on amphibole has indicated
Chillahuita
Complex of volcanic systems in the Puna of the Andes
Chascon (21°53′S 67°54′W / 21.883°S 67.900°W / -21.883; -67.900) Cerro Chillahuita (22°10′S 68°02′W / 22.167°S 68.033°W / -22.167; -68.033) Cerro Galán
Altiplano–Puna volcanic complex
Altiplano–Puna_volcanic_complex
Cerro Porquesa Central Volcanic Zone Rhyodacite Pliocene/Pleistocene Chillahuita Central Volcanic Zone Corona Dome Complex Central Volcanic Zone Andesite
List_of_lava_domes
simultaneously extruded. Altiplano-Puna volcanic complex Cerro Chanka Cerro Chao Chillahuita Corral de Coquena Pastos Grandes Tocorpuri de Silva, S. L.; Self, S.;
Cerro Chascon-Runtu Jarita complex
Cerro_Chascon-Runtu_Jarita_complex
Mountain in Chile
is represented by the 8.3 million years old Sifon ignimbrite, Cerro Chillahuita and Cerro Chao. Linzor and other volcanoes in the neighbourhood are constructed
Linzor
Volcano in Bolivia and Chile
domes Cerro Chanka, Cerro Chao, Cerro Chascon-Runtu Jarita complex, Chillahuita and Tocorpuri were emplaced around 100,000–90,000 years ago. The total
Tocorpuri
(Cerros Bravos-Barros Negros) Chillahuita Lava dome 22°10′S 68°02′W / 22.167°S 68.033°W / -22.167; -68.033 (Chillahuita) Chusmiza Stratovolcano Miocene
List_of_volcanoes_in_Chile
Lava flow complex of Andes volcano Cerro del León
include Cerro Chanca/Pabellon, Cerro Chascon–Runtu Jarita complex, Cerro Chillahuita and La Torta. Cerro Chao lies within a northwest-running belt of volcanoes
Cerro_Chao
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