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Pomerape

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
Pomerape and the saddle below, as seen from south (Parinacota slopes)
Highest point
Elevation6,282 m (20,610 ft)[1]
Prominence950 m (3,120 ft) 
Isolation4 km (2.5 mi) 
Coordinates18°07′33″S 69°07′39″W / 18.12583°S 69.12750°W / -18.12583; -69.12750
Geography
Pomerape
Parent rangeAndes
Geology
Age of rockPleistocene
Mountain typeStratovolcano
Climbing
Easiest routesnow/ice climb

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.

See also edit

References edit

  1. ^ Chilean IGM elevation 2007-09-27 at the Wayback Machine
  2. ^ Map of Curahuara de Carangas Municipality and population data. 2014-11-11 at the Wayback Machine
  3. ^ 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. ISBN 9789401074636.
  4. ^ Carrasco, Jorge F.; Osorio, Roberto; Casassa, Gino (2008-07-01). "Secular trend of the equilibrium-line altitude on the western side of the southern Andes, derived from radiosonde and surface observations". Journal of Glaciology. 54 (186): 545. Bibcode:2008JGlac..54..538C. doi:10.3189/002214308785837002.
  5. ^ Gonzalez-Ferran, Oscar (1994). Volcanes de Chile (in Spanish) (1st ed.). Santiago, Chile: Instituto geografico militar. p. 113. ISBN 9789562020541.
  6. ^ 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. ISBN 9783642773556.
  7. ^ Wörner, G.; Harmon, R. S.; Davidson, J.; Moorbath, S.; Turner, D. L.; McMillan, N.; Nyes, C.; Lopez-Escobar, L.; Moreno, H. (1988-09-01). "The Nevados de Payachata volcanic region (18°S/69°W, N. Chile)" (PDF). Bulletin of Volcanology. 50 (5): 287–303. Bibcode:1988BVol...50..287W. doi:10.1007/BF01073587. hdl:2027.42/47805. ISSN 0258-8900. S2CID 129099050.
  8. ^ 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.
  9. ^ Wörner, Gerhard; Hammerschmidt, Konrad; Henjes-Kunst, Friedhelm; Lezaun, Judith; Wilke, Hans (2000-12-01). "Geochronology (40Ar/39Ar, K-Ar and He-exposure ages) of Cenozoic magmatic rocks from Northern Chile (18-22°S): implications for magmatism and tectonic evolution of the central Andes". Revista Geológica de Chile. 27 (2): 205–240. ISSN 0716-0208.
  10. ^ Gonzalez-Ferran, Oscar (1994). Volcanes de Chile (1st ed.). Santiago, Chile: Instituto geografico militar. p. 113. ISBN 9789562020541.
  11. ^ Biggar, John (2020). The Andes - A Guide for Climbers and Skiers (5th ed.). Scotland: Andes. p. 192. ISBN 978-0-9536087-6-8.


pomerape, stratovolcano, lying, border, northern, chile, bolivia, oruro, department, sajama, province, curahuara, carangas, municipality, part, payachata, complex, volcanoes, together, with, parinacota, volcano, south, name, payachata, means, twins, refers, th. 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 PomerapePomerape and the saddle below as seen from south Parinacota slopes Highest pointElevation6 282 m 20 610 ft 1 Prominence950 m 3 120 ft Isolation4 km 2 5 mi Coordinates18 07 33 S 69 07 39 W 18 12583 S 69 12750 W 18 12583 69 12750GeographyPomerapeBolivia ChileParent rangeAndesGeologyAge of rockPleistoceneMountain typeStratovolcanoClimbingEasiest routesnow ice climb 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 Chungara 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 See also editList of volcanoes in BoliviaReferences edit Chilean IGM elevation Archived 2007 09 27 at the Wayback Machine Map of Curahuara de Carangas Municipality and population data Archived 2014 11 11 at the Wayback Machine 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 ISBN 9789401074636 Carrasco Jorge F Osorio Roberto Casassa Gino 2008 07 01 Secular trend of the equilibrium line altitude on the western side of the southern Andes derived from radiosonde and surface observations Journal of Glaciology 54 186 545 Bibcode 2008JGlac 54 538C doi 10 3189 002214308785837002 Gonzalez Ferran Oscar 1994 Volcanes de Chile in Spanish 1st ed Santiago Chile Instituto geografico militar p 113 ISBN 9789562020541 Worner Gerhard Moorbath Stephen Horn Susanne Entenmann Jurgen 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 ISBN 9783642773556 Worner G Harmon R S Davidson J Moorbath S Turner D L McMillan N Nyes C Lopez Escobar L Moreno H 1988 09 01 The Nevados de Payachata volcanic region 18 S 69 W N Chile PDF Bulletin of Volcanology 50 5 287 303 Bibcode 1988BVol 50 287W doi 10 1007 BF01073587 hdl 2027 42 47805 ISSN 0258 8900 S2CID 129099050 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 Worner Gerhard Hammerschmidt Konrad Henjes Kunst Friedhelm Lezaun Judith Wilke Hans 2000 12 01 Geochronology 40Ar 39Ar K Ar and He exposure ages of Cenozoic magmatic rocks from Northern Chile 18 22 S implications for magmatism and tectonic evolution of the central Andes Revista Geologica de Chile 27 2 205 240 ISSN 0716 0208 Gonzalez Ferran Oscar 1994 Volcanes de Chile 1st ed Santiago Chile Instituto geografico militar p 113 ISBN 9789562020541 Biggar John 2020 The Andes A Guide for Climbers and Skiers 5th ed Scotland Andes p 192 ISBN 978 0 9536087 6 8 Parinacota Global Volcanism Program Smithsonian Institution includes Pomerape This Oruro Department location article is a stub You can help Wikipedia by expanding it vte nbsp This Arica y Parinacota Region location article is a stub You can help Wikipedia by expanding it vte nbsp This South America mountain mountain range or peak related article is a stub You can help Wikipedia by expanding it vte Retrieved from https en wikipedia org w index php title Pomerape amp oldid 1188682324, wikipedia, wiki, book, books, library,

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