Pomerape is a stratovolcano lying on the border of northern Chile and Bolivia (Oruro Department, Sajama Province, Curahuara de Carangas Municipality).[2] It is part of the Payachata complex of volcanoes, together with Parinacota Volcano to the south. The name "Payachata" means "twins" and refers to their appearance.[3] It hosts glaciers down to elevations of 5,300–5,800 metres (17,400–19,000 ft), lower on the northern slope.[4]
Pomerape is a complex of lava domes, accompanied by lava flows which were emplaced atop of the domes.[5] It was active about 200,000 years ago.[6] The lava domes formed first and were later buried by the actual volcanic cone, which unlike the rhyolitic-dacitic domes is formed by hornblende andesite.[7] The "Chungará Andesites" and lava dome complex of Parinacota were laid down at this time.[8] Pomerape is associated with an adventive vent that has erupted mafic magmas. The main cone was last active 106,000 +- 7,000 years ago,[9] the adventive vent is dated to 205,000 ± 24,000 years ago.[10]
Climbing the volcano is alpine grade PD by the east ridge.[11] Harder routes exist on the south face, sometimes on 50+ degree snow/rubble slope. For these routes a camp can be established at 5,300 metres (17,390 ft) at the saddle between Parinacota and Pomerape. Depending on the season, the main difficulty can be penitentes (tall ice-blade needles), which make the ascent physically difficult or impossible.
^Schull, William J. (1990). "Introduction: The Place and the Study". In Schull, William J.; Rothhammer, Francisco (eds.). The Aymara. Studies in Human Biology. Vol. 2. Springer Netherlands. pp. 1–18. doi:10.1007/978-94-009-2141-2_1. ISBN9789401074636.
^Gonzalez-Ferran, Oscar (1994). Volcanes de Chile (in Spanish) (1st ed.). Santiago, Chile: Instituto geografico militar. p. 113. ISBN9789562020541.
^Wörner, Gerhard; Moorbath, Stephen; Horn, Susanne; Entenmann, Jürgen; Harmon, Russel S.; Davidson, Jon P.; Lopez-Escobar, Leopoldo (1994). Reutter, Professor Dr Klaus-Joachim; Scheuber, Dr Ekkehard; Wigger, Dr Peter J. (eds.). Tectonics of the Southern Central Andes. Springer Berlin Heidelberg. p. 81. doi:10.1007/978-3-642-77353-2_5. ISBN9783642773556.
^Hora, J. M.; Singer, B. S.; Worner, G. (2007). "Volcano evolution and eruptive flux on the thick crust of the Andean Central Volcanic Zone: 40Ar/39Ar constraints from Volcan Parinacota, Chile". Geological Society of America Bulletin. 119 (3–4): 343–362. Bibcode:2007GSAB..119..343H. doi:10.1130/b25954.1.