Chutinza

20°54′39″S 68°33′51″W / 20.9108°S 68.5642°W / -20.9108; -68.5642Chutinza is a 5,184 metres (17,008 ft) high^[1] inactive volcano in the Andes, part of the Millunu volcanic complex. In the first stage of its activity, andesite and dacite lava flows with minor pyroclastic components generated a stratovolcano with a crater named Cerro Chutinza Viejo on its northeastern side. Later, lava domes were erupted from the crater (Cerro Tangani), the western flank (Cerro Paja Redonda with a 2 kilometres (1.2 mi) long lava flow) and Cerro Cota 4735.^[2]

References

^ Cerro Perenal (PDF) (Map).
^ Vergara, Hernan. "El Volcanismo Superior En Un Sector Andino Del Norte Grande De Chile (20°45' a 21°00')" (PDF). biblioserver.sernageomin.cl (in Spanish). Arica: Second Chilean Geological Congress. Archived from the original (PDF) on 25 November 2015. Retrieved 22 January 2016.

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[Map-1] Cerro Perenal (PDF) (Map).

[Vergara-2] Vergara, Hernan. "El Volcanismo Superior En Un Sector Andino Del Norte Grande De Chile (20°45' a 21°00')" (PDF). biblioserver.sernageomin.cl (in Spanish). Arica: Second Chilean Geological Congress. Archived from the original (PDF) on 25 November 2015. Retrieved 22 January 2016.

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