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Peinado

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Vignoni, Paula A.; Jurikova, Hana; Schröder, Birgit; Tjallingii, Rik; Córdoba, Francisco E.; Lecomte, Karina L.; Pinkerneil, Sylvia; Grudzinska, Ieva; Schleicher, Anja M.; Viotto, Sofía A.; Santamans, Carla D.; Rae, James W.B.; Brauer, Achim (December 2023). "On the origin and processes controlling
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outgassing appears to occur at the lake. The lake presently has no outflow, but it may have spilled northward into the Salar de Antofalla during periods of higher lake level. Directly north of Laguna Peinado lies another lake, Laguna Turquesa, with an average depth of 6 metres (20 ft) and a
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Laguna Peinado is a 1.2 kilometres (0.75 mi) wide, 3.4 kilometres (2.1 mi) long lake with a mean depth of 4 metres (13 ft)-8 metres (26 ft). Water covers an area of 1.6 square kilometres (0.62 sq mi). It lies at 3,820 metres (12,530 ft) elevation at about
281:; the lava flows have for the most part dark and brown colours. The total volume of the edifice is about 22.4 cubic kilometres (5.4 cu mi), covering an area of 96.2 square kilometres (37.1 sq mi). Claims that the volcano overlies a caldera lack supporting evidence. 1517:
Campeny, López; Escola, P. (2007). "Un verde horizonte en el desierto: producción de cuentas minerales en ámbitos domésticos de sitios agro-pastoriles. Antofagasta de la Sierra. Puna Meridional Argentina". In Nielsen, A.; Rivolta, MC; Seldes, V.; Vázquez, MM; Mercolli, P. (eds.).
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Vignale, Federico A.; Lencina, Agustina I.; Stepanenko, Tatiana M.; Soria, Mariana N.; Saona, Luis A.; Kurth, Daniel; Guzmán, Daniel; Foster, Jamie S.; Poiré, Daniel G.; Villafañe, Patricio G.; Albarracín, Virginia H.; Contreras, Manuel; Farías, María E. (1 January 2022).
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The regional climate is cold and dry, with a mean temperature of 8 °C (46 °F) and large (40 °C (72 °F)) daily temperature fluctuations. Precipitation takes place mainly during the winter months, the region is at the boundary between the
643:. The monogenetic volcanoes just south and north of Peinado developed 210,000 ± 40,000 and 380,000 ± 20,000 years ago, respectively; the flank vent that formed a scoria cone may also be associated with the monogenetic activity rather than Peinado proper. 634:
has yielded ages ranging between 80,000 and 40,000 years ago for the central cone and between 60,000 and 30,000 for the flank vents. Volcanic activity initially built the central cone, before continuing on the flanks. Eruptions have been mostly
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Grosse, Pablo; Guzmán, Silvina R.; Nauret, François; Orihashi, Yuji; Sumino, Hirochika (May 2022). "Central vs. lateral growth and evolution of the < 100 ka Peinado composite volcano, southern Central Volcanic Zone of the Andes".
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that intercepted ascending magma and a single cone. Eventually, the cone reached a size at which further eruptions from the summit were impeded, causing volcanism to shift to the flank vents, which then built up the bulk of Peinado.
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activity. Volcanoes have been observed to remain inactive for ten thousands of years; thus future activity at Peinado is possible. The configuration of volcanic vents suggests that the occurrence of caldera collapse and of
294:; its ignimbrites underlie Peinado and lava flows from Peinado have spilled across its borders on to the caldera floor. On the eastern side, the volcano is bordered by the Sierra de Calalaste. To the north lies the 257:
1,630 metres (5,350 ft) high steep cone, which reaches an elevation of 5,890 metres (19,320 ft) above sea level and features a 240 metres (790 ft) wide and 25 metres (82 ft) deep
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OLIVERA, DANIEL ENZO; TCHILINGUIRIAN, PABLO; CASANOVA MENENDEZ, MARTÍN TOMÁS; PÉREZ, MARTINA INÉS; GRANT, JENNIFER; GENTILE, MARÍA CECILIA; CLUR, ALEJO; DE ZELA, PAULA MIRANDA (2023).
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is possible, and its activity has become more explosive over time. The volcano lies on an eastward younging trend of calderas including Laguna Amarga, and there is evidence of
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Pérez, Martina Inés; Clur, Alejo Adrián; Zela, Paula Miranda De; Olivera, Daniel; Pérez, Martina Inés; Clur, Alejo Adrián; Zela, Paula Miranda De; Olivera, Daniel (May 2023).
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Della Vedova, Micaela; Villafañe, Patricio G.; Cónsole‐Gonella, Carlos; Bahniuk Rumbelsperger, Anelize; Fadel Cury, Leonardo; Horta, Luis R.; Farías, María E. (April 2023).
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reach thicknesses of 30–40 centimetres (12–16 in) and lengths of several 100 metres (330 ft), they extend to Laguna Turquesa. At the southern end of the lake is a
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zone, the Peinado fault, runs from the western side of Salar de Antofalla south along Laguna Peinado to Peinado volcano. Farther south, it may connect to the San Francisco
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when the lake levels were low and conditions more favourable to stromatolite growth than plant development. Recent lake level declines have not prevented the deposition of
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Seggiaro, Raúl E.; Hongn, Fernando D.; Castillo, Alfredo; Pereyra, Fernando Xavier; Villegas, Daniela Claudia; Martínez, Liliana; González, Osvaldo Edgar (2006).
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and other magma-forming processes took place in the magma chamber, yielding the felsic magmas that were erupted from the central vent beginning 40,000 years ago.
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The lakes of the Altiplano have drawn attention in the 21st century owing to the frequently extreme climatic and hydrological conditions they experience.
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ones from the flank vents. The monogenetic volcanoes have erupted basaltic andesite. In the summit region, the rocks have been discoloured presumably by
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caldera just west of Peinado. The climate of the region is cold and dry, but may have been moister in the recent past. North of Peinado lies the
2078:"Spatial variability of the modern radiocarbon reservoir effect in the high-altitude lake Laguna del Peinado (southern Puna Plateau, Argentina)" 383:
surface area of 0.1 square kilometres (0.039 sq mi); the lakes may have been connected before 2005. At the northern end of the basin,
1761:"RESULTADOS INICIALES DEL ANALISIS DEL PRIMER ENTERRATORIO INKAICO CONTEXTUALIZADO EN ANTOFAGASTA DE LA SIERRA (PUNA MERIDIONAL ARGENTINA)" 1989:"Depositional environments of Quaternary lacustrine travertines and stromatolites from high-altitude Andean lakes, northwestern Argentina" 2236: 646:
Presumably, Peinado began its growth as a monogenetic volcano but eruptions became concentrated at a single vent, producing a shallow
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on the mountain. Twelve vents - two of which are buried by lava flows - form cones on its flanks and have produced hundreds of
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Microbial Ecosystems in Central Andes Extreme Environments: Biofilms, Microbial Mats, Microbialites and Endoevaporites
2141:"Short‐term microbialite resurgence as indicator of ecological resilience against crises (Catamarca, Argentine Puna)" 2076:
Vignoni, Paula A.; Córdoba, Francisco E.; Tjallingii, Rik; Santamans, Carla; Lupo, Liliana C.; Brauer, Achim (2023).
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There is evidence of a progressive increase in water levels, followed by a decrease, which may somehow relate to the
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Villafañe, Patricio Guillermo; Cónsole‐Gonella, Carlos; Cury, Leonardo Fadel; Farías, María Eugenia (October 2021).
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mountain sanctuary and may have been used as a source for valuable rocks by pre-Hispanic people. A prehistoric
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Tamberías El Peinado y Laguna Diamante: minería inka y circulaciónd de bienes en la Puna meridional argentina
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Valero-Garcés, Blas; Delgado-Huertas, Antonio; Ratto, Norma; Navas, Ana; Edwards, Larry (1 September 2000).
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The name ("combed" in Spanish) is a reference to its smooth appearance. The first known ascent was by
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of the Central Andes. The region is largely uninhabited, due to the extreme climatic conditions.
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occur on the lowest lake terrace, they display laminated textures and were probably built by
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Valero-Garcés, Blas L; Delgado-Huertas, Antonio; Ratto, Norma; Navas, Ana (30 August 1999).
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of the Andes, which in northern Argentina extends across the Cordillera Occidental and the
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vegetation and underwater plants grow around and in Laguna Peinado, which also features
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mine with well-preserved buildings lies at Tambería El Peinado, close to the volcano.
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Valero-Garcés, Blas L.; Arenas, Concha; Delgado-Huertas, Antonio (9 February 2011).
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occurring in coastal areas and muddy deposits in deeper waters. The carbonates form
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the elemental and isotopic composition of carbonates in hypersaline Andean lakes".
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rates are higher than precipitation. The climate has not been stable during the
2569: 2494: 2034: 1657: 1215: 1110: 438: 395: 379: 302:, the Peinado volcanic field, lies around Peinado. They consist of lava flows, 200: 134: 2121: 2094: 1963: 1601: 1122: 448:
form mounds along 2 kilometres (1.2 mi) of the western lakeshore. Former
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with temperatures reaching 33.13 °C (91.63 °F), which deposit
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Berberián, Eduardo E.; Nielsen, Axel E.; Albeck, María Ester (2001).
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from the Pacific Ocean and isolated drops of cold air hit the area.
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Haselton, Kirk; Hilley, George; Strecker, Manfred R. (March 2002).
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Estudios jeologicos i topograficos del desierto i puna de Atacama
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Producción y Circulación Prehispánicas de Bienes en el Sur Andino
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Jeografía descriptiva de las provincias de Atacama i Antofagasta
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Note: volcanoes are ordered by latitude from north to south
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Perucca, Laura P.; Moreiras, Stella M. (1 January 2009).
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Vitry, Christian (1997). "Arqueología de alta montaña".
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magmas were erupted from the central cone and the more
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Peinado is one of the youngest volcanoes in the area.
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Just west of Peinado lies the eastern margin of the
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Volcanic Landscapes of the Central Andes. Shown are
1402: 974: 524:, and monogenetic volcanoes. Their ages range from 1414: 708:times. What little vegetation there is, is mostly 1831:Seggiaro, R. E.; Hongn, F. D. (12 January 1999). 2892: 1210:Valero-Garcés, Arenas & Delgado-Huertas 2011 1198:Valero-Garcés, Arenas & Delgado-Huertas 2011 1150:Valero-Garcés, Arenas & Delgado-Huertas 2011 1105:Valero-Garcés, Arenas & Delgado-Huertas 2011 1791: 1312: 1622:Journal of Volcanology and Geothermal Research 520:and numerous other calderas with accompanying 242:and about 30 kilometres (19 mi) from the 225: 2230: 1830: 1516: 1502:(in Spanish). Vol. 1. Editorial Brujas. 1468: 1456: 956: 532:; volcanism there has been ongoing since the 2194:Yachayruna Revista de divulgación científica 1876:(in Spanish). Vol. 1. Impr. Barcelona. 394:Lake sediments consist of an alternation of 1794:"Seismic and Volcanic Hazards in Argentina" 1596:. Cham: Springer International Publishing. 1522:(in Spanish). pp. 225–257 – via 567:being erupted more recently. They define a 2237: 2223: 1739:(in Spanish). Impr. Gutenberg – via 723: 2129: 2093: 2042: 1854:Hoja Geológica 2769-II Paso San Francisco 1564: 678: 692:region, where precipitation occurs when 1798:Developments in Earth Surface Processes 2893: 1589: 1185: 265:. There is no perennial snow cover or 2218: 2191: 1871: 1734: 1420: 1408: 980: 739:in 1965, but the mountain features a 2244: 1433:Berberián, Nielsen & Albeck 2001 901:Haselton, Hilley & Strecker 2002 1899:Earth and Planetary Science Letters 1656: 1590:Farías, María Eugenia, ed. (2020). 1276: 791: 779: 625: 214:and large volcanoes, including the 13: 2145:Environmental Microbiology Reports 1993:Canadian Journal of Earth Sciences 1537:Environmental Microbiology Reports 704:, and may have been wetter during 206:The volcano is part of the Andean 14: 2932: 2210: 370:. An additional water source are 1642:10.1016/j.jvolgeores.2022.107532 210:and located within a cluster of 41: 2114:Geochimica et Cosmochimica Acta 1500:Historia argentina prehispánica 478:Sierra Nevada de Lagunas Bravas 246:. Geographically, it is in the 761:List of volcanoes in Argentina 1: 1919:10.1016/S0012-821X(99)00150-8 1810:10.1016/S0928-2025(08)10014-1 782:, Synonyms & Subfeatures. 766: 686:South American Summer Monsoon 552:may be present in the crust. 254: 185:Catamarca Province, Argentina 75:5,890 m (19,320 ft) 2901:Stratovolcanoes of Argentina 195:, surrounded at its foot by 7: 2921:Pleistocene stratovolcanoes 1313:Perucca & Moreiras 2009 754: 238:, close to the border with 226:Geography and geomorphology 10: 2937: 2035:10.1007/s00248-021-01725-8 1490: 653:Fractional crystallization 555:Volcanic rocks are mainly 463: 422:, and they contain fossil 20: 2879: 2836: 2658: 2385: 2252: 2122:10.1016/j.gca.2023.11.032 2095:10.5194/gchron-5-333-2023 1944:Journal of Paleolimnology 1602:10.1007/978-3-030-36192-1 1469:Campeny & Escola 2007 1457:Campeny & Escola 2007 1385:Valero-Garcés et al. 1999 1373:Valero-Garcés et al. 1999 1361:Valero-Garcés et al. 1999 1337:Valero-Garcés et al. 2000 1174:Valero-Garcés et al. 2000 1162:Valero-Garcés et al. 2000 1088:Valero-Garcés et al. 1999 1076:Valero-Garcés et al. 2000 1044:Valero-Garcés et al. 1999 998:Valero-Garcés et al. 1999 957:Seggiaro & Hongn 1999 824:Valero-Garcés et al. 2000 164: 152: 147: 133: 123: 118: 79: 69: 64: 40: 35: 30: 1837:Acta Geológica Hispánica 1735:Muñoz, Santiago (1894). 1663:Global Volcanism Program 1349:Della Vedova et al. 2023 1061:Della Vedova et al. 2023 1027:Della Vedova et al. 2023 170:36,800 ± 3,800 years ago 2157:10.1111/1758-2229.12977 1964:10.1023/A:1008146122074 1911:1999E&PSL.171..253V 1872:Sundt, Lorenzo (1911). 1668:Smithsonian Institution 1549:10.1111/1758-2229.13128 724:Name and human activity 468:Peinado is part of the 317: 2911:Mountains of Argentina 2659:Southern Volcanic Zone 2445:Andagua volcanic field 2253:Northern Volcanic Zone 1688:The Journal of Geology 794:, General Information. 679:Climate and vegetation 458:microbe-produced rocks 362:waters, fed mostly by 49:Nevado Ojos del Salado 2916:Polygenetic volcanoes 2837:Austral Volcanic Zone 2763:Puyehue-Cordón Caulle 2435:Huambo volcanic field 2386:Central Volcanic Zone 1804:. Elsevier: 267–300. 1777:10.24215/18521479e049 1222:Villafañe et al. 2021 1117:Villafañe et al. 2021 658:There are reports of 470:Central Volcanic Zone 402:and travertine, with 342:26.49972°S 68.09222°W 300:monogenetic volcanoes 248:Cordillera Occidental 208:Central Volcanic Zone 21:For the surname, see 18:Mountain in Argentina 2906:Subduction volcanoes 2372:Licto volcanic field 855:Seggiaro et al. 2006 347:-26.49972; -68.09222 36:Volcán del Manantial 1956:2000JPall..24..343V 1700:2002JG....110..211H 1634:2022JVGR..42507532G 1481:OLIVERA et al. 2023 1397:Vignale et al. 2022 1325:Vignoni et al. 2023 1234:Vignale et al. 2022 1138:Vignoni et al. 2023 1010:Vignoni et al. 2023 606:. As is common for 490:Wheelwright caldera 338: /  187:. It consists of a 99: /  2758:Carrán-Los Venados 2703:Nevados de Chillán 2688:Descabezado Grande 1301:Grosse et al. 2022 1289:Grosse et al. 2022 1265:Grosse et al. 2022 1246:Grosse et al. 2022 969:Grosse et al. 2022 945:Grosse et al. 2022 916:Grosse et al. 2022 889:Grosse et al. 2022 872:Grosse et al. 2022 843:Grosse et al. 2022 807:Grosse et al. 2022 639:, but with recent 632:Radiometric dating 575:suite and contain 498:Nevado Tres Cruces 296:Salar de Antofalla 261:with an ephemeral 244:Paso San Francisco 236:Catamarca Province 65:Highest point 2888: 2887: 2698:Nevado de Longaví 2640:Cueros de Purulla 2620:Cordón del Azufre 2282:Nevado del Tolima 2023:Microbial Ecology 1611:978-3-030-36191-4 1445:Pérez et al. 2023 561:basaltic andesite 542:strike-slip fault 518:Cueros de Purulla 253:The volcano is a 174: 173: 103:26.623°S 68.116°W 23:Peinado (surname) 2928: 2883: 2753:Mocho-Choshuenco 2287:Nevado del Huila 2246:Andean volcanoes 2239: 2232: 2225: 2216: 2215: 2205: 2188: 2135: 2133: 2107: 2097: 2072: 2046: 2012: 1999:(8): 1263–1283. 1983: 1934: 1889: 1868: 1858: 1848: 1827: 1788: 1755: 1744: 1731: 1678: 1676: 1674: 1653: 1615: 1586: 1568: 1527: 1513: 1484: 1478: 1472: 1466: 1460: 1454: 1448: 1442: 1436: 1430: 1424: 1418: 1412: 1406: 1400: 1394: 1388: 1382: 1376: 1370: 1364: 1358: 1352: 1346: 1340: 1334: 1328: 1322: 1316: 1310: 1304: 1298: 1292: 1286: 1280: 1279:, Photo Gallery. 1274: 1268: 1262: 1249: 1243: 1237: 1231: 1225: 1219: 1213: 1207: 1201: 1195: 1189: 1183: 1177: 1171: 1165: 1159: 1153: 1147: 1141: 1135: 1120: 1114: 1108: 1102: 1091: 1085: 1079: 1073: 1064: 1058: 1047: 1041: 1030: 1024: 1013: 1007: 1001: 995: 984: 978: 972: 966: 960: 954: 948: 942: 919: 913: 904: 898: 892: 886: 875: 869: 858: 852: 846: 840: 827: 821: 810: 804: 795: 789: 783: 777: 738: 730:Mathias Rebitsch 665:sector collapses 641:explosive events 626:Eruption history 482:Laguna Escondida 385:coastal terraces 353: 352: 350: 349: 348: 343: 339: 336: 335: 334: 331: 256: 230:Peinado lies in 222:Laguna Peinado. 137: 114: 113: 111: 110: 109: 108:-26.623; -68.116 104: 100: 97: 96: 95: 92: 45: 28: 27: 2936: 2935: 2931: 2930: 2929: 2927: 2926: 2925: 2891: 2890: 2889: 2884: 2881: 2875: 2838: 2832: 2660: 2654: 2650:Ojos del Salado 2580:Aguas Calientes 2387: 2381: 2277:Nevado del Ruiz 2254: 2248: 2243: 2213: 2208: 2005:10.1139/e01-014 1856: 1820: 1672: 1670: 1612: 1510: 1493: 1488: 1487: 1479: 1475: 1467: 1463: 1455: 1451: 1443: 1439: 1431: 1427: 1419: 1415: 1407: 1403: 1395: 1391: 1383: 1379: 1371: 1367: 1359: 1355: 1347: 1343: 1335: 1331: 1323: 1319: 1311: 1307: 1299: 1295: 1287: 1283: 1275: 1271: 1263: 1252: 1244: 1240: 1232: 1228: 1220: 1216: 1212:, p. 1280. 1208: 1204: 1200:, p. 1276. 1196: 1192: 1184: 1180: 1172: 1168: 1160: 1156: 1152:, p. 1279. 1148: 1144: 1136: 1123: 1115: 1111: 1107:, p. 1274. 1103: 1094: 1086: 1082: 1074: 1067: 1059: 1050: 1042: 1033: 1025: 1016: 1008: 1004: 996: 987: 979: 975: 967: 963: 955: 951: 943: 922: 914: 907: 899: 895: 887: 878: 870: 861: 853: 849: 841: 830: 822: 813: 805: 798: 790: 786: 778: 774: 769: 757: 732: 726: 688:region and the 681: 671:storage in the 628: 608:stratovolcanoes 502:Ojos del Salado 486:Cerro El Condor 466: 346: 344: 340: 337: 332: 329: 327: 325: 324: 320: 228: 135: 107: 105: 101: 98: 93: 90: 88: 86: 85: 60: 53:Cerro El Cóndor 26: 19: 12: 11: 5: 2934: 2924: 2923: 2918: 2913: 2908: 2903: 2886: 2885: 2880: 2877: 2876: 2874: 2873: 2868: 2863: 2858: 2853: 2848: 2842: 2840: 2834: 2833: 2831: 2830: 2825: 2820: 2815: 2810: 2805: 2800: 2795: 2790: 2785: 2780: 2775: 2770: 2765: 2760: 2755: 2750: 2745: 2740: 2735: 2730: 2725: 2720: 2715: 2710: 2705: 2700: 2695: 2690: 2685: 2680: 2675: 2670: 2664: 2662: 2656: 2655: 2653: 2652: 2647: 2642: 2637: 2632: 2627: 2622: 2617: 2612: 2607: 2602: 2597: 2592: 2587: 2582: 2577: 2572: 2570:Purico complex 2567: 2562: 2557: 2552: 2547: 2542: 2537: 2532: 2527: 2522: 2517: 2512: 2507: 2502: 2497: 2492: 2487: 2482: 2477: 2472: 2467: 2462: 2457: 2452: 2447: 2442: 2437: 2432: 2427: 2422: 2417: 2412: 2407: 2402: 2397: 2391: 2389: 2383: 2382: 2380: 2379: 2374: 2369: 2364: 2359: 2354: 2349: 2344: 2339: 2334: 2329: 2324: 2319: 2314: 2309: 2304: 2299: 2294: 2289: 2284: 2279: 2274: 2269: 2264: 2258: 2256: 2250: 2249: 2242: 2241: 2234: 2227: 2219: 2212: 2211:External links 2209: 2207: 2206: 2196:(in Spanish). 2189: 2151:(5): 659–667. 2136: 2108: 2088:(2): 333–344. 2073: 2013: 1984: 1950:(3): 343–359. 1935: 1905:(2): 253–266. 1890: 1869: 1849: 1828: 1818: 1789: 1756: 1745: 1732: 1708:10.1086/338414 1694:(2): 211–226. 1679: 1654: 1616: 1610: 1587: 1528: 1514: 1508: 1494: 1492: 1489: 1486: 1485: 1473: 1461: 1449: 1447:, p. 111. 1437: 1435:, p. 531. 1425: 1413: 1401: 1389: 1387:, p. 260. 1377: 1375:, p. 259. 1365: 1363:, p. 261. 1353: 1341: 1339:, p. 345. 1329: 1327:, p. 335. 1317: 1305: 1293: 1281: 1269: 1250: 1238: 1226: 1214: 1202: 1190: 1188:, p. 256. 1178: 1176:, p. 356. 1166: 1164:, p. 355. 1154: 1142: 1121: 1109: 1092: 1090:, p. 262. 1080: 1078:, p. 349. 1065: 1048: 1046:, p. 255. 1031: 1014: 1012:, p. 334. 1002: 1000:, p. 254. 985: 973: 961: 959:, p. 239. 949: 920: 905: 903:, p. 217. 893: 876: 859: 847: 828: 826:, p. 344. 811: 796: 784: 771: 770: 768: 765: 764: 763: 756: 753: 725: 722: 718:microbial mats 680: 677: 627: 624: 465: 462: 439:Little Ice Age 380:carbon dioxide 319: 316: 227: 224: 172: 171: 168: 162: 161: 156: 150: 149: 145: 144: 139: 131: 130: 125: 121: 120: 116: 115: 83: 77: 76: 73: 67: 66: 62: 61: 46: 38: 37: 33: 32: 17: 9: 6: 4: 3: 2: 2933: 2922: 2919: 2917: 2914: 2912: 2909: 2907: 2904: 2902: 2899: 2898: 2896: 2878: 2872: 2869: 2867: 2864: 2862: 2859: 2857: 2854: 2852: 2849: 2847: 2844: 2843: 2841: 2835: 2829: 2826: 2824: 2821: 2819: 2816: 2814: 2811: 2809: 2806: 2804: 2801: 2799: 2796: 2794: 2793:Michinmahuida 2791: 2789: 2786: 2784: 2781: 2779: 2776: 2774: 2771: 2769: 2766: 2764: 2761: 2759: 2756: 2754: 2751: 2749: 2746: 2744: 2741: 2739: 2736: 2734: 2731: 2729: 2726: 2724: 2721: 2719: 2716: 2714: 2711: 2709: 2706: 2704: 2701: 2699: 2696: 2694: 2691: 2689: 2686: 2684: 2681: 2679: 2676: 2674: 2671: 2669: 2666: 2665: 2663: 2657: 2651: 2648: 2646: 2643: 2641: 2638: 2636: 2635:San Francisco 2633: 2631: 2628: 2626: 2623: 2621: 2618: 2616: 2613: 2611: 2608: 2606: 2603: 2601: 2598: 2596: 2593: 2591: 2588: 2586: 2583: 2581: 2578: 2576: 2573: 2571: 2568: 2566: 2563: 2561: 2558: 2556: 2553: 2551: 2548: 2546: 2545:Aucanquilcha‎ 2543: 2541: 2538: 2536: 2533: 2531: 2528: 2526: 2523: 2521: 2518: 2516: 2513: 2511: 2508: 2506: 2503: 2501: 2498: 2496: 2493: 2491: 2488: 2486: 2483: 2481: 2478: 2476: 2473: 2471: 2468: 2466: 2463: 2461: 2458: 2456: 2453: 2451: 2448: 2446: 2443: 2441: 2438: 2436: 2433: 2431: 2428: 2426: 2425:Hualca Hualca 2423: 2421: 2418: 2416: 2413: 2411: 2408: 2406: 2403: 2401: 2398: 2396: 2393: 2392: 2390: 2384: 2378: 2375: 2373: 2370: 2368: 2365: 2363: 2360: 2358: 2355: 2353: 2350: 2348: 2345: 2343: 2340: 2338: 2335: 2333: 2330: 2328: 2325: 2323: 2320: 2318: 2315: 2313: 2310: 2308: 2305: 2303: 2300: 2298: 2295: 2293: 2290: 2288: 2285: 2283: 2280: 2278: 2275: 2273: 2270: 2268: 2265: 2263: 2260: 2259: 2257: 2255:(6° N – 3° S) 2251: 2247: 2240: 2235: 2233: 2228: 2226: 2221: 2220: 2217: 2203: 2199: 2195: 2190: 2186: 2182: 2178: 2174: 2170: 2166: 2162: 2158: 2154: 2150: 2146: 2142: 2137: 2132: 2127: 2123: 2119: 2115: 2109: 2105: 2101: 2096: 2091: 2087: 2083: 2082:Geochronology 2079: 2074: 2070: 2066: 2062: 2058: 2054: 2050: 2045: 2040: 2036: 2032: 2028: 2024: 2020: 2014: 2010: 2006: 2002: 1998: 1994: 1990: 1985: 1981: 1977: 1973: 1969: 1965: 1961: 1957: 1953: 1949: 1945: 1941: 1936: 1932: 1928: 1924: 1920: 1916: 1912: 1908: 1904: 1900: 1896: 1891: 1887: 1883: 1879: 1875: 1870: 1866: 1862: 1855: 1850: 1846: 1842: 1838: 1834: 1829: 1825: 1821: 1819:9780444531179 1815: 1811: 1807: 1803: 1799: 1795: 1790: 1786: 1782: 1778: 1774: 1770: 1766: 1762: 1757: 1753: 1752: 1746: 1742: 1738: 1733: 1729: 1725: 1721: 1717: 1713: 1709: 1705: 1701: 1697: 1693: 1689: 1685: 1680: 1669: 1665: 1664: 1659: 1655: 1651: 1647: 1643: 1639: 1635: 1631: 1627: 1623: 1617: 1613: 1607: 1603: 1599: 1595: 1594: 1588: 1584: 1580: 1576: 1572: 1567: 1562: 1558: 1554: 1550: 1546: 1543:(2): 92–108. 1542: 1538: 1534: 1529: 1525: 1521: 1515: 1511: 1505: 1501: 1496: 1495: 1482: 1477: 1470: 1465: 1458: 1453: 1446: 1441: 1434: 1429: 1422: 1417: 1411:, p. 76. 1410: 1405: 1398: 1393: 1386: 1381: 1374: 1369: 1362: 1357: 1351:, p. 93. 1350: 1345: 1338: 1333: 1326: 1321: 1314: 1309: 1303:, p. 20. 1302: 1297: 1291:, p. 13. 1290: 1285: 1278: 1273: 1267:, p. 21. 1266: 1261: 1259: 1257: 1255: 1248:, p. 16. 1247: 1242: 1235: 1230: 1223: 1218: 1211: 1206: 1199: 1194: 1187: 1182: 1175: 1170: 1163: 1158: 1151: 1146: 1139: 1134: 1132: 1130: 1128: 1126: 1118: 1113: 1106: 1101: 1099: 1097: 1089: 1084: 1077: 1072: 1070: 1063:, p. 97. 1062: 1057: 1055: 1053: 1045: 1040: 1038: 1036: 1029:, p. 96. 1028: 1023: 1021: 1019: 1011: 1006: 999: 994: 992: 990: 983:, p. 42. 982: 977: 970: 965: 958: 953: 946: 941: 939: 937: 935: 933: 931: 929: 927: 925: 918:, p. 22. 917: 912: 910: 902: 897: 890: 885: 883: 881: 873: 868: 866: 864: 856: 851: 844: 839: 837: 835: 833: 825: 820: 818: 816: 809:, p. 14. 808: 803: 801: 793: 788: 781: 776: 772: 762: 759: 758: 752: 750: 746: 742: 736: 731: 721: 719: 715: 711: 707: 703: 699: 695: 691: 687: 676: 674: 670: 666: 661: 656: 654: 649: 648:magma chamber 644: 642: 638: 633: 623: 621: 617: 613: 609: 605: 601: 600:orthopyroxene 597: 593: 590: 586: 582: 581:clinopyroxene 578: 574: 573:calc-alkaline 570: 566: 562: 558: 553: 551: 547: 543: 539: 535: 531: 527: 523: 519: 515: 511: 507: 503: 499: 495: 491: 487: 483: 479: 475: 471: 461: 459: 455: 454:cyanobacteria 451: 450:stromatolites 447: 446:Microbialites 442: 440: 435: 433: 429: 425: 421: 417: 413: 409: 405: 401: 397: 392: 390: 386: 381: 377: 373: 369: 365: 361: 357: 351: 315: 313: 309: 305: 301: 297: 293: 290: 289:Laguna Amarga 287: 282: 280: 276: 272: 268: 264: 260: 259:summit crater 251: 249: 245: 241: 237: 233: 223: 221: 217: 216:Laguna Amarga 213: 209: 204: 202: 199:erupted from 198: 194: 193:summit crater 190: 189:volcanic cone 186: 182: 181:stratovolcano 178: 169: 167: 166:Last eruption 163: 160: 159:Stratovolcano 157: 155: 154:Mountain type 151: 146: 143: 140: 138: 132: 129: 126: 122: 117: 112: 84: 82: 78: 74: 72: 68: 63: 58: 54: 50: 44: 39: 34: 29: 24: 16: 2743:Quetrupillán 2629: 2605:Llullaillaco 2470:Huaynaputina 2202:Academia.edu 2197: 2193: 2185:ResearchGate 2183:– via 2148: 2144: 2113: 2085: 2081: 2044:11336/148472 2026: 2022: 2009:ResearchGate 2007:– via 1996: 1992: 1947: 1943: 1931:Academia.edu 1929:– via 1902: 1898: 1886:Google Books 1884:– via 1873: 1836: 1824:Academia.edu 1822:– via 1801: 1797: 1768: 1764: 1750: 1741:Google Books 1736: 1728:ResearchGate 1726:– via 1691: 1687: 1671:. Retrieved 1661: 1625: 1621: 1592: 1540: 1536: 1524:Academia.edu 1519: 1499: 1476: 1471:, p. 3. 1464: 1459:, p. 5. 1452: 1440: 1428: 1423:, p. 2. 1416: 1404: 1399:, p. 8. 1392: 1380: 1368: 1356: 1344: 1332: 1320: 1308: 1296: 1284: 1272: 1241: 1236:, p. 5. 1229: 1224:, p. 7. 1217: 1205: 1193: 1181: 1169: 1157: 1145: 1140:, p. 5. 1119:, p. 5. 1112: 1083: 1005: 976: 971:, p. 9. 964: 952: 947:, p. 3. 896: 891:, p. 6. 874:, p. 4. 857:, p. 3. 850: 845:, p. 2. 787: 775: 741:pre-Hispanic 727: 682: 657: 645: 629: 622:alteration. 620:hydrothermal 554: 514:Cerro Blanco 494:Falso Azufre 467: 443: 436: 393: 321: 308:scoria cones 283: 275:pyroclastics 252: 229: 205: 176: 175: 136:Parent range 15: 2839:(49°–55° S) 2823:Mate Grande 2673:Tupungatito 2661:(33°–46° S) 2540:Olca-Paruma 2535:Irruputuncu 2525:Tata Sabaya 2465:Pichu Pichu 2395:Quimsachata 2388:(14°–27° S) 2272:Cerro Bravo 2131:10023/29245 2029:(1): 1–17. 1839:: 227–242. 1186:Farías 2020 733: [ 714:Salt-loving 702:Pleistocene 698:Evaporation 694:cold fronts 610:, the more 604:plagioclase 577:phenocrysts 522:ignimbrites 510:Cerro Torta 420:wackestones 378:. Volcanic 372:hot springs 364:groundwater 345: / 263:crater lake 201:flank vents 106: / 81:Coordinates 2895:Categories 2783:Hornopirén 2768:Casablanca 2738:Villarrica 2733:Sollipulli 2693:Cerro Azul 2565:Licancabur 2560:Sairecabur 2520:Guallatiri 2510:Parinacota 2490:Purupuruni 2400:Auquihuato 2367:Tungurahua 2362:Chimborazo 2322:Reventador 2297:Doña Juana 1765:Relaciones 1628:: 107532. 1509:987945250X 1421:Vitry 1997 1409:Sundt 1911 1315:, Table 4. 981:Muñoz 1894 767:References 690:westerlies 530:Quaternary 412:packstones 404:limestones 376:travertine 354:. It is a 333:68°05′32″W 330:26°29′59″S 312:tuff rings 271:lava flows 197:lava flows 94:68°06′58″W 91:26°37′23″S 2803:Corcovado 2723:Lonquimay 2683:Calabozos 2668:Tupungato 2645:Incahuasi 2610:Lastarria 2590:Chiliques 2430:Sabancaya 2410:Sara Sara 2327:Pichincha 2262:Paipa-Iza 2181:235348046 2165:1758-2229 2104:2628-3719 2069:253768636 2053:1432-184X 1980:129052389 1972:1573-0417 1927:0012-821X 1882:654477717 1865:0328-2333 1845:2173-6537 1785:1852-1479 1771:: 13–14. 1716:0022-1376 1658:"Peinado" 1650:247416244 1583:252694965 1557:1758-2229 749:aragonite 712:grasses. 660:fumarolic 569:potassium 546:lineament 538:Oligocene 506:Incahuasi 474:Altiplano 432:oncolites 428:ostracods 416:rudstones 368:meltwater 356:salt lake 232:Argentina 220:salt lake 128:Argentina 119:Geography 71:Elevation 2871:Fueguino 2856:Aguilera 2808:Mentolat 2718:Callaqui 2555:Zapaleri 2485:Yucamane 2480:Tutupaca 2450:Chachani 2420:Coropuna 2415:Solimana 2357:Quilotoa 2352:Cotopaxi 2347:Illiniza 2332:Antisana 2173:34089237 2061:33730193 1724:18111576 1673:14 April 1575:36192831 1566:10103866 1277:GVP 2023 792:GVP 2023 780:GVP 2023 755:See also 637:effusive 589:titanium 557:andesite 408:micrites 360:alkaline 286:Pliocene 267:glaciers 212:calderas 124:Location 2846:Lautaro 2798:Chaitén 2778:Calbuco 2713:Copahue 2630:Peinado 2615:Lazufre 2600:Socompa 2505:Taapaca 2475:Ticsani 2317:Cayambe 2307:Azufral 2302:Galeras 2267:Romeral 1952:Bibcode 1907:Bibcode 1696:Bibcode 1630:Bibcode 1491:Sources 706:glacial 596:olivine 563:, with 526:Miocene 464:Geology 424:diatoms 400:calcite 396:organic 389:wetland 292:caldera 191:with a 177:Peinado 148:Geology 31:Peinado 2866:Burney 2861:Reclus 2851:Viedma 2828:Hudson 2788:Huequi 2773:Osorno 2728:Llaima 2708:Antuco 2595:Aracar 2585:Lascar 2575:Pacana 2550:Azufre 2530:Isluga 2500:Tacora 2495:Casiri 2460:Ubinas 2440:Ampato 2405:Firura 2377:Sangay 2312:Chiles 2292:Puracé 2179:  2171:  2163:  2102:  2067:  2059:  2051:  1978:  1970:  1925:  1880:  1863:  1843:  1816:  1783:  1722:  1714:  1648:  1608:  1581:  1573:  1563:  1555:  1506:  745:copper 710:steppe 612:felsic 592:oxides 571:-rich 565:dacite 534:Eocene 398:muds, 279:scoria 59:, 2010 2748:Lanín 2678:Maipo 2625:Galán 2515:Lauca 2455:Misti 2342:Soche 2337:Aliso 2177:S2CID 2065:S2CID 1976:S2CID 1857:(PDF) 1720:S2CID 1646:S2CID 1579:S2CID 737:] 673:crust 669:magma 616:mafic 550:Magma 358:with 304:maars 240:Chile 179:is a 142:Andes 2818:Macá 2169:PMID 2161:ISSN 2100:ISSN 2057:PMID 2049:ISSN 1968:ISSN 1923:ISSN 1878:OCLC 1861:ISSN 1841:ISSN 1814:ISBN 1781:ISSN 1712:ISSN 1675:2023 1606:ISBN 1571:PMID 1553:ISSN 1504:ISBN 747:and 602:and 585:iron 559:and 426:and 418:and 366:and 318:Lake 310:and 277:and 2813:Cay 2153:doi 2126:hdl 2118:doi 2090:doi 2039:hdl 2031:doi 2001:doi 1960:doi 1915:doi 1903:171 1806:doi 1773:doi 1704:doi 1692:110 1638:doi 1626:425 1598:doi 1561:PMC 1545:doi 579:of 528:to 234:'s 183:in 57:ISS 2897:: 2175:. 2167:. 2159:. 2149:13 2147:. 2143:. 2124:. 2116:. 2098:. 2084:. 2080:. 2063:. 2055:. 2047:. 2037:. 2027:83 2025:. 2021:. 1997:38 1995:. 1991:. 1974:. 1966:. 1958:. 1948:24 1946:. 1942:. 1921:. 1913:. 1901:. 1897:. 1835:. 1812:. 1802:13 1800:. 1796:. 1779:. 1769:48 1767:. 1763:. 1718:. 1710:. 1702:. 1690:. 1686:. 1666:. 1660:. 1644:. 1636:. 1624:. 1604:. 1577:. 1569:. 1559:. 1551:. 1541:15 1539:. 1535:. 1253:^ 1124:^ 1095:^ 1068:^ 1051:^ 1034:^ 1017:^ 988:^ 923:^ 908:^ 879:^ 862:^ 831:^ 814:^ 799:^ 735:de 720:. 675:. 598:, 594:, 583:, 516:, 512:, 508:, 504:, 500:, 496:, 492:, 488:, 484:, 480:, 434:. 414:, 410:, 391:. 306:, 255:c. 51:, 2238:e 2231:t 2224:v 2204:. 2198:1 2187:. 2155:: 2134:. 2128:: 2120:: 2106:. 2092:: 2086:5 2071:. 2041:: 2033:: 2011:. 2003:: 1982:. 1962:: 1954:: 1933:. 1917:: 1909:: 1888:. 1867:. 1847:. 1826:. 1808:: 1787:. 1775:: 1743:. 1730:. 1706:: 1698:: 1677:. 1652:. 1640:: 1632:: 1614:. 1600:: 1585:. 1547:: 1526:. 1512:. 1483:. 587:- 536:- 25:.

Index

Peinado (surname)

Nevado Ojos del Salado
Cerro El Cóndor
ISS
Elevation
Coordinates
26°37′23″S 68°06′58″W / 26.623°S 68.116°W / -26.623; -68.116
Argentina
Parent range
Andes
Mountain type
Stratovolcano
Last eruption
stratovolcano
Catamarca Province, Argentina
volcanic cone
summit crater
lava flows
flank vents
Central Volcanic Zone
calderas
Laguna Amarga
salt lake
Argentina
Catamarca Province
Chile
Paso San Francisco
Cordillera Occidental
summit crater

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