Monte Pissis

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Monte Pissis
Monte Pissis.jpg
Monte Pissis from the northeast
Highest point
Elevation 6,793 m (22,287 ft)
Prominence 2,145 m (7,037 ft) [1][A]
Listing
Coordinates 27°45′21″S 68°47′57″W / 27.75583°S 68.79917°W / -27.75583; -68.79917Coordinates: 27°45′21″S 68°47′57″W / 27.75583°S 68.79917°W / -27.75583; -68.79917[1]
Geography
Monte Pissis is located in Argentina
Monte Pissis
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

Monte Pissis is an extinct volcano on the border of La Rioja and Catamarca provinces, Argentina, 25 km (16 mi) from the Chilean border. The mountain is the third-highest in the Western Hemisphere, and is located about 550 km (340 mi) north of Aconcagua. 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 there is an extensive glacier (with crevasses, which is unique in the region)

Elevation[edit]

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).[2]

Geology[edit]

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.[3] Volcanism in the area ceased about 2 million years ago.[4]

Monte Pissis, Cerro Bonete Chico and Incapillo form a large volcanic complex that is among the highest in the world.[5] Incapillo formed after Monte Pissis had ceased erupting, and hydrothermal activity at Incapillo may continue to this day.[6]

Climbing[edit]

Until recently, this mountain had received very little attention. The first successful recorded ascent was achieved in 1937 by Polish climbers Osiecki and Szczepanski. The mountain was not climbed again until 1985.

The opening of mining in the area has resulted in the construction of basic roads in the last 15 years. This has developed the tourism 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 neighboring Chile is also possible but involves a longer way.

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 required as 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.

Main glacier on Monte Pissis.

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 4,500 m (14,800 ft) several days of hike 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.

See also[edit]

References[edit]

  1. ^ a b "Argentina and Chile North: Ultra-Prominences". Peaklist. 2006. 
  2. ^ "Ojos del Salado, el volcán más Alto del Mundo" (in Spanish). Desnivel. 22 May 2007. 
  3. ^ Kay, Suzanne Mahlburg; Mpodozis, Constantino; Gardeweg, Moyra (2014-01-01). "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. 
  4. ^ Mahlburg Kay, Suzanne; Mpodozis, Constantino (2002-04-01). "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. 
  5. ^ Goss, A. R.; Kay, S. M. (2003-12-01). "Termination of a Central Andean arc: The Chemical Evolution of the Bonete-Incapillo Volcanic Complex, Argentina". AGU Fall Meeting Abstracts. 41. Bibcode:2003AGUFM.S41D0123G. 
  6. ^ Goss, A. R.; Kay, S. M.; Mpodozis, C.; Singer, B. S. (2009-07-20). "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. 

Bibliography[edit]

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

Notes[edit]

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

External links[edit]