凱火山
45°03′45″S 72°59′09″W / 45.06250°S 72.98583°W
凱火山是智利的火山，位於該國南部伊瓦涅斯將軍艾森大區，鄰近馬卡火山，海拔高度2,090米，山體在更新世時期由玄武岩和英安岩組成。
參考資料
- "Cay". Global Volcanism Program. Smithsonian Institution.
- D'Orazio, M.; Tamponia, M.; Tonarinib, S.; González-Ferránd, O.; Lahsend, A.; Omarinie, R. (August 2003). "The Quaternary calc-alkaline volcanism of the Patagonian Andes close to the Chile triple junction: geochemistry and petrogenesis of volcanic rocks from the Cay and Maca volcanoes (not, vert, similar45°S, Chile)". Journal of South American Earth Sciences. 16 (4): 219–242. Bibcode:2003JSAES..16..219D. doi:10.1016/S0895-9811(03)00063-4.
- José A. Naranjo; Charles R. Stern (December 2004). "Holocene tephrochronology of the southernmost part (42°30'-45°S) of the Andean Southern Volcanic Zone". Revista Geológica de Chile. 31 (2): 225–240. doi:10.4067/S0716-02082004000200003.
- M D'Orazio; F Innocenti; P Manetti; M Tamponi; S Tonarini; O González-Ferrán; A Lahsen; R Omarini (August 2003). "The Quaternary calc-alkaline volcanism of the Patagonian Andes close to the Chile triple junction: geochemistry and petrogenesis of volcanic rocks from the Cay and Maca volcanoes (∼45°S, Chile)". Journal of South American Earth Sciences. 16 (4): 219–242. Bibcode:2003JSAES..16..219D. doi:10.1016/S0895-9811(03)00063-4.
 | 這是一篇與智利地理相關的小作品。您可以透過編輯或修訂擴充其內容。 |