Tupungatito
Tupungatito Volcano | |
---|---|
South Volcanic Zone | |
Last eruption | 1987[2] |
Volcán Tupungatito is the northernmost historically active
Tupungatito lies in proximity to the border between
Volcanism is caused by the subduction of the Nazca Plate underneath the South America Plate. Tupungatito formed less than 100,000 years ago and has had a number of historical eruptions, the latest in 1987, which were mostly small explosive eruptions. Presently, the volcano features an acidic crater lake and numerous fumaroles. Renewed eruptions could induce volcanic ash falls in Argentina and dangerous mudflows in Chile.
Name and history
The name Tupungatito was assigned to the volcano by
There was speculation about the existence of a volcano in the Andes near Santiago already during the
Geography and geomorphology
Tupungatito is located in the Chilean
The volcano features a 5 kilometres (3.1 mi) wide caldera with an erupted volume of 5 cubic kilometres (1.2 cu mi) and one
Glaciers and hydrology
Above 5,400 metres (17,700 ft) elevation, the volcano is covered with
The ice and snow cover on Tupungatito is an important source of water for the rivers in the region
Geology
Regional
Off the coast of South America, the
The SVZ is a 1,400 kilometres (870 mi) long and, depending on latitude, up to 200 kilometres (120 mi) wide chain of
Local
The volcano lies on a c. 50 kilometres (31 mi) thick
The volcano forms a volcanic group with Tupungato[16] and another peak, 6,000 metres (20,000 ft) high Nevado Sin Nombre.[29] Tupungato and Nevado Sin Nombre formed during the late and early Pleistocene, respectively,[13] and are presently inactive.[10] The caldera is to a large degree formed by rocks from Nevado Sin Nombre.[11] 6,019 metres (19,747 ft) high Nevado de los Piuquenes is a fourth volcano in this group and overlaps with Nevado Sin Nombre.[29] Below 4,700 metres (15,400 ft) elevation, Tupungatito is underlaid by an eroded volcano whose rocks resemble Tupungato.[1]
Composition
Tupungatito has erupted rocks ranging from
Climate
The mean annual temperature on Tupungatito is about −15.5 °C (4.1 °F)
Glaciers have alternatively advanced and retreated during the 20th century.[32] There is some uncertainty as sometimes snow cover is confused for glacial ice.[15] As of 2016[update] ice covers an area of 112.84 ± 3.66 square kilometres (43.57 ± 1.41 sq mi), down from 119.89 ± 8.36 square kilometres (46.29 ± 3.23 sq mi) in 1986;[33] this encompasses the ice cover of Tupungatito and other volcanoes in the area.[34] Volcanic eruptions have not significantly altered the ice extent.[33]
Eruption history
Tupungatito is about 55,000
Historical activity
Records of activity at Tupungatito go back to 1646
In 1835,
Eruptions at Tupungatito frequently deposited
Present-day status and threats
The volcano is
Since 2012, the volcano is monitored by the Southern Volcanological Observatory of the Andes.
See also
Notes
- ^ Tupungato is the northernmost volcano of the SVZ.[27]
- ^ A 1987 landslide in the region generated a mudflow down the Rio Colorado, which killed 41 people and damaged roads, hydropower plants and water supply infrastructure of Santiago, is unrelated to Tupungatito and a seismic trigger is questionable.[46]
References
- ^ a b c GVP 2021, General Information.
- ^ Barrera V. 1974, p. 188.
- ^ Jahn 1939, p. 17.
- ^ a b Steffen 1927, p. 514.
- ^ Steffen 1927, p. 511.
- ^ Steffen 1927, p. 513.
- ^ Steffen 1927, p. 515.
- ^ a b c Flores & Jara 2018, p. 6.
- ^ a b c d e f g h i SERNAGEOMIN 2017, p. 1.
- ^ a b c d e f Flores & Jara 2018, p. 8.
- ^ a b c d e Bertin & Carolina 2015, p. 1.
- ^ a b c Muñoz 1983, p. 837.
- ^ a b c d Reinthaler et al. 2019, p. 547.
- ^ a b c d Flores & Jara 2018, p. 7.
- ^ Casassa, Rodríguez & Blindow 2014, p. 730.
- ^ a b Potocki et al. 2015, p. A-5.
- ^ a b c Potocki et al. 2014, p. A-5.
- ^ Smolka & Volkheimer 2000, pp. 143–145.
- ^ Bundschuh et al. 2012, p. 16.
- ^ a b NARANJO & MORENO 1991, p. 3.
- ^ a b c Moreno & Gibbons 2007, p. 154.
- ^ a b Stern 2004, p. 161-206.
- ^ a b Moreno & Gibbons 2007, p. 156.
- ^ a b Piquer et al. 2019, pp. 223–239.
- ^ a b NARANJO & MORENO 1991, p. 5.
- ^ a b c d Bertin & Carolina 2015, p. 3.
- ^ a b c Bertin & Carolina 2015, p. 2.
- ^ Masiokas et al. 2009, p. 248.
- ^ a b Reinthaler et al. 2019, p. 551.
- ^ Reinthaler et al. 2019, Supplementary Figure S10.
- ^ a b c SEGEMAR 2021.
- ^ Bertin & Carolina 2015, pp. 1–2.
- ^ Bosch, Stern & Moreiras 2015, p. 639.
- ^ Espizua & Bigazzi 1998, p. 760.
- ^ Flores & Jara 2018, p. 30.
- ^ a b Steffen 1905, p. 45.
- ^ Darwin 1835, p. 310.
- ^ Abascal 1941, p. 78.
- ^ Casertano 1962, p. 218.
- ^ Brüggen 1950, p. 65.
- ^ de Ragone et al. 2004, p. 189.
- ^ GVP 2021, Bulletin Reports.
- ^ Jay et al. 2013, p. 164.
- ^ Barrientos 2018, p. 471.
- ^ Flores & Jara 2018, p. 9.
- ^ Edwards, Kochtitzky & Battersby 2020, p. 13.
- ^ González-Muzzio & Vidal 2020, p. 11.
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