Apacheta-Aguilucho volcanic complex

Apacheta-Aguilucho volcanic complex is a volcanic complex in Chile. It consists of two volcanoes Cerro Apacheta and Cerro Aguilucho, which are constructed mainly by lava flows and surrounded by outcrops of lava. A sector collapse and its landslide deposit are located on Apacheta's eastern flank. Two lava domes are associated with the volcanic complex, Chac-Inca and Pabellón.

Apacheta-Aguilucho volcanic complex
Highest point
Elevation5,557 m (18,232 ft) [1]
Coordinates [1]
Geography
Apacheta-Aguilucho volcanic complex

The volcanic complex was active from the Miocene to the Pleistocene, but ongoing fumarolic activity has been observed and a geothermal system is present. A geothermal power plant was being built in 2015 and became active in late 2017.

Geomorphology and geography

Apacheta-Aguilucho lies in northern Chile, close to the border with Bolivia.[2] The city of Calama lies 105 kilometres (65 mi) southwest of Apacheta-Aguilucho,[3] but with the exception of mining-associated infrastructure the area is remote and uninhabited.[2]

The volcano is part of the Central Volcanic Zone of the Andes. The Central Volcanic Zone further includes the Altiplano-Puna volcanic complex, which between 10 and 1 million years ago was the source of large ignimbrite eruptions[3] that produced over 15,000 cubic kilometres (3,600 cu mi) of rock;[4] after that it produced lava flows and lava domes like Cerro Chao and geothermal fields such as El Tatio and Sol de Mañana,[3] accompanied by a decreased production of volcanic material.[4] The Altiplano-Puna volcanic complex is underpinned by a magmatic body that appears to be a batholith.[5] Volcanic activity is the consequence of the subduction of the Nazca Plate beneath the South America Plate.[6] Aside from volcanic activity, crustal shortening has resulted in a thickened crust since about 35 million years ago.[5]

Apacheta-Aguilucho is a volcanic complex formed by two volcanoes,[1] Cerro Apacheta and Cerro Aguilucho, both composite volcanoes;[7] with the highest summit of the complex reaching a height of 5,557 metres (18,232 ft).[1] The northern Aguilucho volcano and the southern Apacheta volcano are in their central portions formed by rhyolitic lava flows, with the surrounding edifice formed by andesitic-dacitic lavas. An andesitic lahar and pyroclastic flow crops out south and east of Apacheta,[8] which as the oldest part of the edifice is heavily eroded.[2] North and east of the complex, the two lava domes Chac-Inca and Cerro Pabellón[8] form the youngest part of the volcano.[2]

Moraines are encountered both west-southwest of Apacheta and east of the Chac-Inca dome,[8] and traces of glacial erosion are observed on the Aguilucho crater region.[9] The moraines developed during the last glacial maximum.[10]

Geothermal manifestations

The volcano is fumarolically active on Apacheta's northern[11] and eastern slopes[12] as well as on the summit.[13] Two fumaroles on the northern flank of Apacheta produce superheated steam at a high output; the gas has a composition typical of geothermal system fumaroles, with some differences.[11]

Apacheta-Aguilucho has a geothermal system and the chemistry of fumarole gases suggests that Apacheta-Aguilucho features an active magma system at depth. Drilling has found temperatures of over 200 °C (392 °F) at 500 metres (1,600 ft) depth.[3] This fumarolic activity has resulted in hydrothermal alteration of many parts of the volcano;[1] this activity has generated a sulfur deposit on the west flank of Aguilucho.[7] The mine Mina Aguilucho is located on Aguilucho's western flank.[11] The geothermal activity was discovered in 1999.[6]

The discovery of steam during the drilling of a freshwater well in the 1990s led to investigations by ENAP and UNOCAL in the area and the discovery of the fumaroles. In 2002, a joint enterprise by ENAP and CODELCO obtained the permission to explore the area, but while a geothermal system was discovered political questions about ENAP's involvement derailed the project.[2]

Another joint enterprise this time including the Italian ENEL performed further research in the area between 2006-2007, and obtained a permit to exploit the system in 2009.[2] The joint enterprise started the geothermal power project Cerro Pabellón, and in 2015 the construction of two power plants with a projected output of 24 MW each started, to be completed in 2017-2018.[14] The plant was inaugurated by the Chilean president Michelle Bachelet on 12 September 2017, becoming either the first[15] or the second (after Copahue) geothermal power station in South America.[6]

Sector collapse

A landslide deposit extends 4.5 kilometres (2.8 mi) away from the volcanic complex on its eastern flank. The landslide deposit covers a surface of about 3 square kilometres (1.2 sq mi),[1] and a large collapse scar with signs of hydrothermal alteration faces the western end of the landslide.[9] In its upper part, the deposit is bordered to the north and south by levees.[16] Downslope, the deposit consists at first of a lobate structure that east of the Pabellón dome grades into a more hummocky deposit. The deposit is increasingly dominated by hydrothermally altered material farther east, while the hummocks consist of lava blocks.[17] The material of the landslide deposit itself features both solid blocks and a finer matrix.[18] Rocks involved in the landslide include both andesitic and dacitic lavas and hydrothermally altered material. The landslide deposit is confined between two older lava flows.[1]

Sector collapses like the one at Apacheta-Aguilucho have been observed on other volcanoes (such as Mount St Helens during its 1980 eruption), and they result in characteristic landslide deposits known as debris avalanche deposits; these feature hummock-like hills and often levees. Such collapses occur for different reasons for each event and are fairly common; in the Central Andes alone 14 volcanoes feature deposits of such collapses.[19] Such deposits commonly feature a stratigraphy that resembles that of the source edifice, as well as jigsaw-like cracks in rocks that form when rocks disintegrate during the collapse and sliding.[20]

In the case of Apacheta-Aguilucho, it is likely that the sector collapse was triggered by hydrothermal alteration of the edifice that weakened its structure until it failed, and its path was likely influenced by regional tectonics.[21] After the edifice had failed, the landslide moved eastward until it was deflected by older topography; the material became increasingly fragmented.[22]

Geology

Off the west coast of South America, the Nazca Plate subducts beneath the South America Plate in the Peru-Chile Trench. This subduction process is responsible for volcanism in the Central Andes, which occurs at distances of 250–300 kilometres (160–190 mi) from the trench.[1]

Two major fault systems are found close to Apacheta-Aguilucho. The first is the major regional Calama-Olacapato-El Toro fault, the second fault system runs from neighbouring Inacaliri volcano northwest of Apacheta-Aguilucho towards the southeast, where it forms the Pabellóncito graben;[1] the volcanic complex is built within that graben.[3] The Pabellóncito fault system was active during the Pleistocene; the activity of these regional fault systems appears to be a consequence of tectonic regime changes during the early Pleistocene, which drove extensional tectonics in the area.[10] Northwest of Apacheta-Aguilucho, the axis of the graben is buried beneath other volcanoes starting with Cerro del Azufre.[23]

The basement beneath Apacheta-Aguilucho is of Eocene to Miocene age. It consists of various volcanic and sedimentary formations[23][1] including eroded volcanoes,[3] and it is in part covered by 7.5 million years old ignimbrites.[1]

Composition

Apacheta-Aguilucho has principally erupted andesite, dacite and rhyolite.[1] These rocks define a potassium-rich calc-alkaline suite which contains amphibole, biotite, clinopyroxene, iron-titanium oxides, orthopyroxene, olivine, plagioclase, quartz, sanidine and titanite. Olivine is often altered to clay, goethite and hematite.[24] The magmas appear to derive from the Altiplano-Puna magmatic complex volcanic body and underwent fractional crystallization and other geochemical processes before erupting.[25]

Eruption history

The volcanic complex is of Pliocene to Pleistocene age[7] and developed over several different stages. In the first stage, the so-called Aguilucho ignimbrite consisting of moderately welded, white-to-pink pyroclastic flows was emplaced 7.5 ± 0.6 million years ago and andesitic lava flows 6.7 ± 0.3 million years ago. Subsequently, more lava flows were emplaced, consisting of blocky dacite.[12]

The Apacheta and Aguilucho volcanoes were constructed consecutively. Apacheta consists of lava flows and pyroclastic material made out of andesite, and its crater is covered by pyroclastic flows and a 2.5 kilometres (1.6 mi) long rhyolitic lava flow. Aguilucho is constructed by lava flows. Finally, several lava flow fields were emplaced together with the lava domes Pabellón and Chac-Inca.[12] 1,204,000 ± 33,000 years ago an ignimbrite named Aguilucho ignimbrite was erupted[26] from the Apacheta volcano.[5]

Lava flows on Apacheta-Aguilucho have been dated to 910,000 ± 140,000 and 700,000 ± 200,000 years before present,[1] with one lava flow being dated to 652,000 ± 12,000 years ago.[26] The date of the sector collapse is not known with certainty but was probably after the last lava flow was emplaced on Apacheta-Aguilucho.[21]

Dating of Chac-Inca has produced an age of 140,000 ± 80,000 years before present. Different dates have been obtained on Cerro Pabellón: Potassium-argon dating yields an age of 130,000 - 80,000 years before present, while argon-argon dating has yielded an age of 50,000 ± 10,000 years before present.[12]

See also

References
  1. Godoy et al. 2017, p. 137.
  2. Bona & Coviello 2016, p. 51.
  3. Mercado et al. 2009, p. 1.
  4. Taussi et al. 2019, p. 179.
  5. Taussi et al. 2019, p. 181.
  6. Maza et al. 2018, p. 4.
  7. Urzua et al. 2002, p. 1.
  8. Godoy et al. 2017, p. 138.
  9. Godoy et al. 2017, p. 141.
  10. Mercado et al. 2009, p. 3.
  11. Urzua et al. 2002, p. 4.
  12. Mercado et al. 2009, p. 2.
  13. Maza et al. 2018, p. 6.
  14. Bona & Coviello 2016, p. 52.
  15. "Cerro Pabellón, la planta geotérmica chilena pionera en Sudamérica y a mayor altura del mundo" (in Spanish). Santiago: Emol. 17 September 2017. Retrieved 13 December 2017.
  16. Godoy et al. 2017, p. 140.
  17. Godoy et al. 2017, p. 139.
  18. Godoy et al. 2017, p. 138,139.
  19. Godoy et al. 2017, p. 136.
  20. Godoy et al. 2017, p. 142.
  21. Godoy et al. 2017, p. 144.
  22. Godoy et al. 2017, p. 145.
  23. Urzua et al. 2002, p. 3.
  24. Taussi et al. 2019, p. 186.
  25. Taussi et al. 2019, p. 195.
  26. Taussi et al. 2019, p. 180.

Sources
  • Bona, Paolo; Coviello, Manlio (April 2016). "Valoración y gobernanza de los proyectos geotérmicos en América del Sur: una propuesta metodológica" (PDF). repositorio.cepal.org (in Spanish). Economic Commission for Latin America and the Caribbean. pp. 1–178. Retrieved 12 December 2017.CS1 maint: ref=harv (link)
  • Godoy, Benigno; Rodríguez, Inés; Pizarro, Marcela; Rivera, Germain (November 2017). "Geomorphology, lithofacies, and block characteristics to determine the origin, and mobility, of a debris avalanche deposit at Apacheta-Aguilucho Volcanic Complex (AAVC), northern Chile". Journal of Volcanology and Geothermal Research. 347: 136–148. doi:10.1016/j.jvolgeores.2017.09.008. ISSN 0377-0273.CS1 maint: ref=harv (link)
  • Maza, S. N.; Collo, G.; Morata, D.; Lizana, C.; Camus, E.; Taussi, M.; Renzulli, A.; Mattioli, M.; Godoy, B.; Alvear, B.; Pizarro, M.; Ramírez, C.; Rivera, G. (2018). "Clay mineral associations in the clay cap from the Cerro Pabellón blind geothermal system, Andean Cordillera, Northern Chile". Clay Minerals. 53 (2): 117–141. doi:10.1180/clm.2018.9. ISSN 0009-8558.CS1 maint: ref=harv (link)
  • Mercado, J.L.; Ahumada, S.; Aguilera, F.; Medina, E.; Renzulli, A.; Piscaglia, F. (November 2009). "Geological and Structural Evolution of Apacheta-Aguilucho Volcanic Complex (AAV C), Northern Chile" (PDF). SERNAGEOMIN. Santiago: 12th Chilean Geological Congress. pp. 1–4. Retrieved 12 December 2017.CS1 maint: ref=harv (link)
  • Taussi, Marco; Godoy, Benigno; Piscaglia, Filippo; Morata, Diego; Agostini, Samuele; Le Roux, Petrus; González-Maurel, Osvaldo; Gallmeyer, Guillermo; Menzies, Andrew; Renzulli, Alberto (March 2019). "The upper crustal magma plumbing system of the Pleistocene Apacheta-Aguilucho Volcanic Complex area (Altiplano-Puna, northern Chile) as inferred from the erupted lavas and their enclaves". Journal of Volcanology and Geothermal Research. 373: 179–198. doi:10.1016/j.jvolgeores.2019.01.021.CS1 maint: ref=harv (link)
  • Urzua, Luis; Powell, Tom; Cumming, William B.; Dobson, Patrick (2002). "Apacheta, a new geothermal prospect in Northern Chile" (PDF). eScholarship. Lawrence Berkeley National Laboratory. Retrieved 13 December 2017.CS1 maint: ref=harv (link)
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