Apacheta-Aguilucho volcanic complex
Apacheta-Aguilucho volcanic complex | |
---|---|
Highest point | |
Elevation | 5,557 m (18,232 ft)[1] |
Coordinates | 21°50′S 68°10′W / 21.833°S 68.167°W[1] |
Geography | |
Apacheta-Aguilucho volcanic complex (also known as Cerro Pabellón
The volcanic complex was active from the
Geography and geomorphology
The Apacheta-Aguilucho volcanic complex lies in northern Chile, close to the border with
The volcanic complex is part of the
The volcanic complex
Apacheta-Aguilucho is a volcanic complex formed by two volcanoes,
Geothermal manifestations
Apacheta volcano is
Apacheta-Aguilucho has a geothermal system and the chemistry of fumarole gases suggests that Apacheta-Aguilucho features an active
The Pabellón geothermal system was discovered in 1999,
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),
Sector collapses like the one at the Apacheta-Aguilucho volcanic complex have been observed on other volcanoes (such as
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.[34] After the edifice had failed, the landslide moved eastward until it was deflected by older topography; the material became increasingly fragmented.[35]
Geology
Off the west coast of South America, the
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[4] and the eruption of Pabellón was influenced by the graben faults, which allowed magma to reach the surface. The Pabellóncito fault system was active during the Pliocene[23] until present-day, with seismic activity recorded in 2017 and 2020.[36] 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,[15] or of gravitational spreading of the crust under the weight of volcanoes in the area.[37] Northwest of Apacheta-Aguilucho, the axis of the graben is buried beneath other volcanoes starting with Cerro del Azufre[38] which form a northwest–southeast alignment[22] known as Inacaliri lineament.[39]
The basement beneath Apacheta-Aguilucho is of Eocene to Miocene age. It consists of various volcanic and sedimentary formations[38][1] including eroded volcanoes,[4] and it is in part covered by 7.5 million years old ignimbrites.[1]
Composition
Apacheta-Aguilucho has principally erupted
Eruption history
The volcanic complex is of Pliocene to Pleistocene age[11] 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.[17]
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.[17] 1,204,000 ± 33,000 years ago an ignimbrite named Aguilucho ignimbrite was erupted[42] from the Apacheta volcano.[8]
Apacheta grew between about 1.024 and 0.9 million years ago and Aguilucho between 0.7 and 0.6 million years ago.
Dating of Chac-Inca has produced an age of 140,000 ± 80,000 years before present. Different dates have been obtained on Cerro Pabellón:
Geothermal power production
The discovery of steam during the drilling of a freshwater well in the 1990s led to investigations by
Another joint enterprise this time including the Italian
The Cerro Pabellón project is expected to produce 340
Notes
See also
References
- ^ a b c d e f g h i j k l m Godoy et al. 2017, p. 137.
- ^ a b c Morata et al. 2020, p. 1.
- ^ a b c d e f Bona & Coviello 2016, p. 51.
- ^ a b c d e f Mercado et al. 2009, p. 1.
- ^ a b c d Taussi et al. 2019, p. 2.
- ^ Taussi et al. 2019, p. 7.
- ^ a b Taussi et al. 2019, p. 179.
- ^ a b c Taussi et al. 2019, p. 181.
- ^ a b c Lobos Lillo et al. 2023, p. 2.
- ^ a b c Maza et al. 2018, p. 4.
- ^ a b c Urzua et al. 2002, p. 1.
- ^ a b c Godoy et al. 2017, p. 138.
- ^ S2CID 133979654.
- ^ a b Godoy et al. 2017, p. 141.
- ^ a b Mercado et al. 2009, p. 3.
- ^ a b c Urzua et al. 2002, p. 4.
- ^ a b c d Mercado et al. 2009, p. 2.
- ^ Maza et al. 2018, p. 6.
- ^ a b c Morata et al. 2020, p. 4.
- ^ Maza et al. 2021, p. 5.
- ^ a b Godoy et al. 2022, p. 2.
- ^ a b Morata et al. 2020, p. 2.
- ^ a b c d Morata et al. 2020, p. 3.
- ^ Taussi et al. 2019, p. 9.
- ^ Taussi et al. 2019, p. 3.
- ^ Morata et al. 2020, p. 6.
- ^ Taussi et al. 2019, p. 12.
- ^ Taussi et al. 2021, p. 2.
- ^ Godoy et al. 2017, p. 140.
- ^ Godoy et al. 2017, p. 139.
- ^ Godoy et al. 2017, p. 138,139.
- ^ Godoy et al. 2017, p. 136.
- ^ Godoy et al. 2017, p. 142.
- ^ a b Godoy et al. 2017, p. 144.
- ^ Godoy et al. 2017, p. 145.
- ^ Lobos Lillo et al. 2023, p. 6.
- ^ Taussi et al. 2021, p. 4.
- ^ a b Urzua et al. 2002, p. 3.
- ^ ISSN 0717-7305. Archived from the original(PDF) on June 29, 2021. Retrieved 20 August 2021.
- ^ Taussi et al. 2019, p. 186.
- ^ Taussi et al. 2019, p. 195.
- ^ a b Taussi et al. 2019, p. 180.
- ^ Godoy et al. 2022, p. 17.
- ^ Lobos Lillo et al. 2023, p. 9.
- ^ Bona & Coviello 2016, p. 52.
- ^ Bona & Coviello 2016, p. 30.
- ^ "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.
- ^ Maza et al. 2021, p. 1.
- ^ S2CID 224860830.
- ISBN 9789567052479 – via ResearchGate.
- ISBN 9780323886680.
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: 1–178. Retrieved 12 December 2017.
- 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. ISSN 0377-0273.
- Godoy, Benigno; Taussi, Marco; González-Maurel, Osvaldo; Hübner, Darío; Lister, James; Sellés, Daniel; le Roux, Petrus; Renzulli, Alberto; Rivera, Germain; Morata, Diego (March 2022). "Evolution of the Azufre volcano (northern Chile): Implications for the Cerro Pabellón Geothermal Field as inferred from long lasting eruptive activity". Journal of Volcanology and Geothermal Research. 423: 107472. S2CID 246051408.
- Lobos Lillo, Diego; Delgado, Francisco; Pritchard, Matt E.; Cardona, Carlos; Franco, Luis; Pedreros, Gabriela; Amigo, Alvaro (September 2023). "Documenting surface deformation at the first geothermal power plant in South America (Cerro Pabellón, Chile) by satellite InSAR time-series". Journal of Volcanology and Geothermal Research. 441: 107869. S2CID 259906824.
- 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. S2CID 134830461.
- Maza, Santiago N.; Collo, Gilda; Morata, Diego; Taussi, Marco; Vidal, Jeanne; Mattioli, Michele; Renzulli, Alberto (1 November 2021). "Active and fossil hydrothermal zones of the Apacheta volcano: Insights for the Cerro Pabellón hidden geothermal system (Northern Chile)". Geothermics. 96: 102206. ISSN 0375-6505.
- 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. Archived from the original(PDF) on October 11, 2015. Retrieved 12 December 2017.
- Morata, Diego; Maza, Santiago; Vidal, Jeanne; Taussi, Marco; Renzulli, Alberto; Mattioli, Michele; Pizarro, Marcela; Camus, Estefanía; Godoy, Benigno; Alvear, Bernardita; Rivera, Germain (2020). Hydrothermal Alteration in Cerro Pabellón Geothermal Field: from Surface and Drill Core Data to Conceptual Model (PDF). Proceedings World Geothermal Congress. Reykjavik, Iceland.
- 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. S2CID 135345626.
- Taussi, Marco; Nisi, Barbara; Pizarro, Marcela; Morata, Diego; Veloso, Eugenio A.; Volpi, Gianni; Vaselli, Orlando; Renzulli, Alberto (15 October 2019). "Sealing capacity of clay-cap units above the Cerro Pabellón hidden geothermal system (northern Chile) derived by soil CO2 flux and temperature measurements". Journal of Volcanology and Geothermal Research. 384: 1–14. S2CID 199096742.
- Taussi, Marco; Nisi, Barbara; Vaselli, Orlando; Maza, Santiago; Morata, Diego; Renzulli, Alberto (January 2021). "Soil CO2 flux and temperature from a new geothermal area in the Cordón de Inacaliri Volcanic Complex (northern Chile)". Geothermics. 89: 101961. ISSN 0375-6505.
- 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.
External links
- Cerro Pabellon Geothermal Project (Apacheta). UNFCC (Report).
- Cristian Andrés Gutiérrez Villalobos. Ficha del Proyecto: Central Geotérmica Cerro Pabellón (Report). Forma de Presentación: Estudio de Impacto Ambiental (in Spanish). SGA.