Monte Pissis

Monte Pissis
Monte Pissis
	Monte Pissis from the northeast
Highest point
Elevation	6,792 m (22,283 ft)
Prominence	2,145 m (7,037 ft)
Listing	Seven Third Summits; Ultra;
Coordinates	27°45′19″S 68°47′57″W / 27.75528°S 68.79917°W
Geography
	Monte Pissis Location in Argentina
Location	La Rioja and Catamarca provinces, Argentina
Parent range	Andes
Geology
Mountain type	Stratovolcano
Climbing
First ascent	1937 by Osiecki and Jan Alfred Szczepański
Easiest route	Hike, east side

Monte Pissis is an extinct volcano on the border of the La Rioja and Catamarca provinces in Argentina, 25 km (16 mi) to the east of the Chilean border and about 550 km (340 mi) north of Aconcagua. The mountain is the third-highest in the Western Hemisphere. Monte Pissis is named after Pedro José Amadeo Pissis, a French geologist who worked for the Chilean government. Due to its location in the Atacama Desert, the mountain has very dry conditions but features an extensive glacier, with crevasses, which is unique in the region. The peak is the highest summit on Earth without a permanent glacier.^[4]

Elevation

A 1994 Argentine expedition claimed —using GPS technology available at the time— that the elevation of Monte Pissis was 6,882 m (22,579 ft), higher than Ojos del Salado. Ten years later, with the use of higher precision systems, several other surveys proved that those measurements were inaccurate: in 2005, an Austrian team performed a DGPS survey of Pissis' summit and found the elevation to be 6,793 m (22,287 ft). In 2006 an international expedition surveyed the height on the summit, and found results in agreement with an elevation around 6,800 m (22,300 ft). This was later confirmed by a 2007 Chilean-Argentine-European expedition, which surveyed both Ojos del Salado and Monte Pissis and provisionally found the former to be 6,891 m (22,608 ft) and the latter 6,793 m (22,287 ft).^[5]^[6]

Geology

Monte Pissis is a large andesitic-dacitic volcanic centre. It was formed between 6.6 and 6.2 million years ago. Like Cerro Bonete Chico it is one of the large volcanic complexes formed at that time over a deforming Nazca slab.^[7] Volcanism in the area ceased about 2 million years ago.^[8]

Monte Pissis, Cerro Bonete Chico and Incapillo form a large volcanic complex that is among the highest in the world.^[9] Incapillo formed after Monte Pissis had ceased erupting, and hydrothermal activity at Incapillo may continue to this day.^[10]

Climbing

Until recently, this mountain had received very little attention. The first successful recorded ascent was made in 1937 by Polish climbers Stefan Osiecki and Jan Alfred Szczepański of the Second Polish Andean Expedition.^[11] The mountain was not climbed again until 1985.

The advent of mining in the area has resulted in the construction of basic roads in the last 15 years. This has helped tourism to develop in the Atacama Desert, and now more people ascend the mountain, usually with a previous stop in Fiambalá to organise the climb. Approaching it from neighbouring Chile is also possible but involves a longer route.

As the mountain is very high and remote, a long approach is required but the ascent is easy and does not require any specific climbing skill. Nevertheless, warm clothing and good shoes are essential, as the temperature during the night can drop as low as −30 °C (−22 °F) and winds can be very strong. Usually most teams ascend the peak during December to March, the warmest period of the year.

The peak is one of the most heavily glaciated peaks in the Atacama Desert, although the glaciated area starts only at 5,900 m (19,400 ft), and the size of the glacier is small compared to the overall surface of the mountain.

From the base of the mountain at 4,500 m (14,800 ft), several days of hiking are required. The summit is usually reached directly from a high camp at 5,900 m (19,400 ft) at the edge of the glacier.

References

^ "Phillipe Reuter: "El Ojos del Salado es 100 metros más alto que el Pissis"". Archived from the original on 2011-07-08. Retrieved 2007-05-24.
^ "Argentina and Chile North: Ultra-Prominences". Andes Specialists. 2020. Archived from the original on 2020-04-07. Retrieved 2020-04-11.
^ "Andean Mountains - All above 5000m". Archived from the original on 2020-04-07. Retrieved 2020-04-11.
^ "Do All Mountains Wear Snowcaps?". wonderopolis.org/wonder. Wonderopolis.
^ "Ojos del Salado, el volcán más Alto del Mundo" (in Spanish). Desnivel. 22 May 2007. Archived from the original on 7 January 2014. Retrieved 1 August 2013.
^ "Phillipe Reuter: "El Ojos del Salado es 100 metros más alto que el Pissis"". Archived from the original on 8 July 2011. Retrieved 11 April 2020.
^ Kay, Suzanne Mahlburg; Mpodozis, Constantino; Gardeweg, Moyra (1 January 2014). "Magma sources and tectonic setting of Central Andean andesites (25.5–28°S) related to crustal thickening, forearc subduction erosion and delamination". Geological Society, London, Special Publications. 385 (1): 303–334. Bibcode:2014GSLSP.385..303K. doi:10.1144/SP385.11. ISSN 0305-8719. S2CID 129489335. Archived from the original on 16 August 2017. Retrieved 13 January 2017.
^ Mahlburg Kay, Suzanne; Mpodozis, Constantino (1 April 2002). "Magmatism as a probe to the Neogene shallowing of the Nazca plate beneath the modern Chilean flat-slab". Journal of South American Earth Sciences. Flat-Slab Subduction in the Andes. 15 (1): 52. Bibcode:2002JSAES..15...39M. doi:10.1016/S0895-9811(02)00005-6. hdl:10533/173279.
^ Goss, A. R.; Kay, S. M. (1 December 2003). "Termination of a Central Andean arc: The Chemical Evolution of the Bonete-Incapillo Volcanic Complex, Argentina". AGU Fall Meeting Abstracts. 41: S41D–0123. Bibcode:2003AGUFM.S41D0123G.
^ Goss, A. R.; Kay, S. M.; Mpodozis, C.; Singer, B. S. (20 July 2009). "The Incapillo Caldera and Dome Complex (~ 28° S, Central Andes): A stranded magma chamber over a dying arc". Journal of Volcanology and Geothermal Research. 184 (3–4): 389–404. Bibcode:2009JVGR..184..389G. doi:10.1016/j.jvolgeores.2009.05.005.
^ Hartemann, Frederic; Hauptman, Robert (15 June 2005). The Mountain Encyclopedia: An A to Z Compendium of Over 2,250 Terms, Concepts, Ideas, and People. Taylor Trade Publishing. p. 141. ISBN 978-1-4617-0331-0. Archived from the original on 24 August 2023. Retrieved 17 November 2020.

Bibliography

Darack, Ed (2001). Wild Winds: Adventures in the Highest Andes. Cordee / DPP. ISBN 978-1884980817.

Notes

^ The prominence value given here is based on an elevation of 6,795 m (22,293 ft)

External links

KML file (edit • help)

Template:Attached KML/Monte Pissis

KML is not from Wikidata

[1] "Phillipe Reuter: "El Ojos del Salado es 100 metros más alto que el Pissis"". Archived from the original on 2011-07-08. Retrieved 2007-05-24.

[peaklist-2] "Argentina and Chile North: Ultra-Prominences". Andes Specialists. 2020. Archived from the original on 2020-04-07. Retrieved 2020-04-11.

[4] "Andean Mountains - All above 5000m". Archived from the original on 2020-04-07. Retrieved 2020-04-11.

[5] "Do All Mountains Wear Snowcaps?". wonderopolis.org/wonder. Wonderopolis.

[6] "Ojos del Salado, el volcán más Alto del Mundo" (in Spanish). Desnivel. 22 May 2007. Archived from the original on 7 January 2014. Retrieved 1 August 2013.

[7] "Phillipe Reuter: "El Ojos del Salado es 100 metros más alto que el Pissis"". Archived from the original on 8 July 2011. Retrieved 11 April 2020.

[8] Kay, Suzanne Mahlburg; Mpodozis, Constantino; Gardeweg, Moyra (1 January 2014). "Magma sources and tectonic setting of Central Andean andesites (25.5–28°S) related to crustal thickening, forearc subduction erosion and delamination". Geological Society, London, Special Publications. 385 (1): 303–334. Bibcode:2014GSLSP.385..303K. doi:10.1144/SP385.11. ISSN 0305-8719. S2CID 129489335. Archived from the original on 16 August 2017. Retrieved 13 January 2017.

[9] Mahlburg Kay, Suzanne; Mpodozis, Constantino (1 April 2002). "Magmatism as a probe to the Neogene shallowing of the Nazca plate beneath the modern Chilean flat-slab". Journal of South American Earth Sciences. Flat-Slab Subduction in the Andes. 15 (1): 52. Bibcode:2002JSAES..15...39M. doi:10.1016/S0895-9811(02)00005-6. hdl:10533/173279.

[10] Goss, A. R.; Kay, S. M. (1 December 2003). "Termination of a Central Andean arc: The Chemical Evolution of the Bonete-Incapillo Volcanic Complex, Argentina". AGU Fall Meeting Abstracts. 41: S41D–0123. Bibcode:2003AGUFM.S41D0123G.

[11] Goss, A. R.; Kay, S. M.; Mpodozis, C.; Singer, B. S. (20 July 2009). "The Incapillo Caldera and Dome Complex (~ 28° S, Central Andes): A stranded magma chamber over a dying arc". Journal of Volcanology and Geothermal Research. 184 (3–4): 389–404. Bibcode:2009JVGR..184..389G. doi:10.1016/j.jvolgeores.2009.05.005.

[12] Hartemann, Frederic; Hauptman, Robert (15 June 2005). The Mountain Encyclopedia: An A to Z Compendium of Over 2,250 Terms, Concepts, Ideas, and People. Taylor Trade Publishing. p. 141. ISBN 978-1-4617-0331-0. Archived from the original on 24 August 2023. Retrieved 17 November 2020.

[3] The prominence value given here is based on an elevation of 6,795 m (22,293 ft)

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v t e Seven Third Summits
Asia	Kangchenjunga (8,586 m or 28,169 ft)
South America	Monte Pissis (6,795 m or 22,293 ft)
North America	Pico de Orizaba (5,636 m or 18,491 ft)
Europe	Shkhara (5,193 m or 17,037 ft) or Dom (4,545 m or 14,911 ft)
Africa	Mawenzi (5,149 m or 16,893 ft)
Antarctica	Mount Shinn (4,661 m or 15,292 ft)
Oceania	Puncak Trikora (4,750 m or 15,584 ft)
Australia	Mount Twynam (2,195 m or 7,201 ft)