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Sierra Chichinautzin
The Sierra Chichinautzin volcanic field, also known as ''El Pedegral'', is located in the Trans-Mexican Volcanic Belt, approximately from where the Cocos Plate subducts beneath the North American Plate.〔(Heterogeneous magmas of the Quaternary Sierra Chichinautzin Volcanic Field (central Mexico): the role of an amphibole-bearing mantle and magmatic evolution processes ). Magmas heterogéneos del campo volcánico Cuaternario de la Sierra de Chichinautzin (México central): el papel de un manto con anfíbol y los procesos de evolución magmática. Revista Mexicana de Ciencias Geológicas, 2008, volumen 25, número 2: 197-216. Retrieved 2011-09-05〕
==Description==
According to The Smithsonian Institution's Global Volcanism Program, "The massive Chichinautzin volcanic field covers a long, East-West trending area immediately south of central Mexico City." 〔(Chichinautzin ). Global Volcanism Program, The Smithsonian Institution, National Museum of Natural History, Washington, D.C. Retrieved 2011-09-05〕
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