Chutinza
Appearance
From Wikipedia, the free encyclopedia
20°54′39′′S 68°33′51′′W / 20.9108°S 68.5642°W / -20.9108; -68.5642 Chutinza 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
[edit ]- ↑ 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.
Stub icon
This volcanology article is a stub. You can help Wikipedia by adding missing information.
Retrieved from "https://en.wikipedia.org/w/index.php?title=Chutinza&oldid=1117500478"