The volcano rises 1,600–1,700 metres (5,200–5,600 ft) above the surrounding terrain.[6] Suni K'ira is the source of an ignimbrite,[3] and it features a caldera at the intersection of several faults.[6] The volcano features cirques which were formerly considered to be craters, leading to the belief that eruptions occurred during the Holocene.
^ abcFernández, A.C.; Hörmann, P.K.; Kussmaul, S.; Meave, J.; Pichler, H.; Subieta, T. (1 September 1973). "First petrologic data on young volcanic rocks of SW-Bolivia". Tschermaks Mineralogische und Petrographische Mitteilungen. 19 (3): 160–162. doi:10.1007/BF01167425. ISSN0369-1497.
^ abKussmaul, S.; Hörmann, P.K.; Ploskonka, E.; Subieta, T. (1 April 1977). "Volcanism and structure of southwestern Bolivia". Journal of Volcanology and Geothermal Research. 2 (1): 87–88. doi:10.1016/0377-0273(77)90016-6.