Aguas Calientes Volcano or Cerro Aguas Calientes, also called Simba,[2] is a cone-shaped
stratovolcano located 5 kilometres (3 mi) east of the
Lascar volcano and 10 kilometres (6.2 mi) north of
Laguna Lejía, Chile.[2] It is located within a 500 square kilometres (190 sq mi) area where the Cordón de Puntas Negras and the Cordón Chalviri volcanic chains intersect.[2] The volcano is constructed from
andesite and
dacite containing
hornblende and also
anhydrite and its pyroclastics are all older than Lascar.[3][4] It has a diameter of about 7 kilometres (4.3 mi).[5] Some xenoliths of calc-alkaline material are found in Aguas Calientes lavas, and magma mixing has generated lavas containing andesite inclusions in dacites. One eruption of Aguas Calientes postdates the first centre of Lascar and was originally linked to the Lascar Piedras Grandes eruption, before sampling on the deposits of this eruption indicated a relationship with the Lascar volcano itself.[6] Effusion of lava ceased after the cone was built.[7] One summit lava flow may be of Holocene age,[8] but no evidence of historical activity is found (González-Ferrán 1985).
The volcano has been affected by
glaciation. Glacial U-shaped valleys are found on the northern and western flanks, giving the volcano some angular patterns. One valley with glacial features and a subglacial river channel at 4,650 metres (15,260 ft) altitude is found on the northern flank. It extends down to the valley north of Aguas Calientes and intersects the youngest lavas of the volcano.[4]
Aguas Calientes has a well formed summit crater.[8] A small
crater lake is found within the Aguas Calientes summit crater, making it one of the highest lakes in the world[9] at an altitude of 5,870 metres (19,260 ft). The lake has a surface area of 2,500 square metres (27,000 sq ft)[2] and is tinged red from a population of microorganisms.[5] The lake water is acidic and is frequently influenced by activity from Lascar, with winds carrying sulfuric acid and water vapour clouds to the crater lake. Precipitation was measured at 146 millimetres per year (5.7 in/year) with most precipitation falling during the winter months,[2] and strong UV irradiation.[10] The lake has a bacterial ecosystem that is primarily reliant on photosynthesis but may also be influenced by hydrothermal activity from Aguas Calientes volcano.[11] Research has found only limited numbers of bacterial taxa and a large number of DNA sequences that can't be identified as known phylogenetic groups.[12] The lake has been studied as a possible terrestrial analogy to
Mars.[2]
^Matthews, S. J.; Jones, A. P.; Beard, A. D. (1 October 1994). "Buffering of melt oxygen fugacity by sulphur redox reactions in calc-alkaline magmas". Journal of the Geological Society. 151 (5): 815–823.
Bibcode:
1994JGSoc.151..815M.
doi:
10.1144/gsjgs.151.5.0815.
S2CID128416319.
^
ab"Volcanoes". High Lakes 2006 Expedition. Retrieved 14 January 2016.
^Matthews, S. J.; Jones, A. P.; Gardeweg, M. C. (1 April 1994). "Lascar Volcano, Northern Chile; Evidence for Steady-State Disequilibrium". Journal of Petrology. 35 (2): 401–432.
Bibcode:
1994JPet...35..401M.
doi:
10.1093/petrology/35.2.401.
^Escudero, Lorena;
Chong, Guillermo; Demergasso, Cecilia; Farías, María Eugenia; Cabrol, Nathalie A.; Grin, Edmond; Minkley Jr., Edwin; Yu, Yeoungeob (1 October 2007). Hoover, Richard B; Levin, Gilbert V; Rozanov, Alexei Y; Davies, Paul C. W (eds.). "Investigating microbial diversity and UV radiation impact at the high-altitude Lake Aguas Calientes, Chile". Instruments, Methods, and Missions for Astrobiology X. 6694: 66940Z.
Bibcode:
2007SPIE.6694E..0ZE.
doi:
10.1117/12.736970.
hdl:11336/92123.
S2CID123492194.
Sources
González-Ferrán, Oscar (1995). Volcanes de Chile. Santiago, Chile: Instituto Geográfico Militar. p. 640.
ISBN956-202-054-1. (in Spanish; also includes volcanoes of Argentina, Bolivia, and Peru)