The volcano is formed from two volcanic cones. The younger of which may be of Holocene age and is constructed in the middle of a caldera marked by a semilunar shape.[3]: 141 Thanks to heavy erosion, lavas and eruption products are mostly found in peripheral parts of the edifice, while in the central area a deep-grounded crystalline core is exposed.[4]: 150 A breach 3.5 kilometres (2.2 mi) wide and 5.5 kilometres (3.4 mi) long with an azimuth of 139° lies in the volcano, whose summit has a maximum slope of 25°.[1] The volcano forms a lineament with Saxani and Isluga.[5]
The creeks named Qhamiña (Camiña) and on the western side Waywasi (Guayhuase) originate on the volcano.[6]: 101 Sulfur deposits on the volcano were exploited by indigenous people.[7]: 63
^Jiménez, J.A.; Cano, M.J. (2008). "Taxonomic assessment of Didymodon pruinosus (Mitt.) R.H. Zander (Bryophyta, Pottiaceae) a poorly known South American taxon". Nova Hedwigia. 87 (1): 146. doi:10.1127/0029-5035/2008/0087-0145. ISSN0029-5035.
^Avila-Salinas, Waldo (1991). "Petrologic and tectonic evolution of the Cenozoic volcanism in the Bolivian western Andes". Andean Magmatism and Its Tectonic Setting. Geological Society of America Special Papers. Vol. 265. p. 248. doi:10.1130/SPE265-p245. ISBN0-8137-2265-9. ISSN0072-1077.
^Guillermo Eduardo Billinghurst (1893). La irrigación en Tarapacá (in Spanish). Imprenta y Librería Ercilla.