29:
427:
age occur on the southern side of the volcano. The small volume of the main
Quetrupillán edifice and the widespread vents may reflect the interaction between the volcano and the Liquiñe-Ofqui fault, which generated secondary vents whose location was controlled by the Liquiñe-Ofqui fault, the
712:
Reports exist of eruptions during the 19th century, one eruption was reported in 1872. Explosive activity has a recurrence interval of about 1,200 years, which given the age of the last event carries significant implications with regards to the volcanic hazard of
Quetrupillán.
1291:
Brahm, Raimundo; Parada, Miguel Angel; Morgado, Eduardo; Contreras, Claudio; McGee, Lucy Emma (May 2018). "Origin of
Holocene trachyte lavas of the Quetrupillán volcanic complex, Chile: Examples of residual melts in a rejuvenated crystalline mush reservoir".
410:
that occupy a surface of 400 square kilometres (150 sq mi). These subsidiary vents include the scoria cone
Huililco, the Volcanes de Llancahue and the Volcanoes de Reyehueico. There are in total 16 lateral vents, of which 12 are found in a
366:. The Cordillera El Mocho and Quinquilil volcanoes are likewise situated on this alignment, both are deeply eroded composite volcanoes of small dimensions. Other volcanoes in the Southern Volcanic Zone have similar alignments, such as
1758:
Pavez, Maximiliano; Brasse, Heinrich; Kapinos, Gerhard; Díaz, Daniel; Lara, Luis E.; Schill, Eva (July 2023). "Magma storage and transfer in the
Villarrica volcanic chain, South Chile: MT insights into volcano-tectonic interactions".
1430:
Brahm, R.; Parada, M. Á.; Morgado, E. E.; Contreras, C. (2015-12-01). "Pre-eruptive rejuvenations of crystalline mush by reservoir heating: the case of trachy-dacitic lavas of
Quetrupillán Volcanic Complex, Chile (39º30' lat. S)".
545:
Based on the composition, it has been inferred that the magma reservoir of
Quetrupillán contained a mush of crystals, from which magma was repeatedly mobilized following the injection of fresh magmas that reheated the mush.
983:
Rivera Merino, Maria Nicol; Sepúlveda
Arriagada, Leslie Viviana; Silva Carrasco, Claudia Andrea; Rivera Merino, Maria Nicol; Sepúlveda Arriagada, Leslie Viviana; Silva Carrasco, Claudia Andrea (December 2022).
1335:
Daniele, Linda; Taucare, Matías; Viguier, Benoît; Arancibia, Gloria; Aravena, Diego; Roquer, Tomás; Sepúlveda, Josefa; Molina, Eduardo; Delgado, Antonio; Muñoz, Mauricio; Morata, Diego (1 November 2020).
1588:
289:
provinces. Towns close to
Quetrupillán are Catripulli, Currarehue and Puesco. It is considered Chile's 21st most dangerous volcano. The volcano and its neighbours form part of the
398:
is unconfirmed. The entire edifice has a north-south elongated shape and covers a ground surface of 107 square kilometres (41 sq mi). The volcano contains a field of
1485:
Fontijn, Karen; Rawson, Harriet; Van Daele, Maarten; Moernaut, Jasper; Abarzúa, Ana M.; Heirman, Katrien; Bertrand, Sébastien; Pyle, David M.; Mather, Tamsin A. (2016-04-01).
331:
of the Andes. The rate and geometry of subduction has varied over time. During the last six million years, the subduction process has been oblique and as a consequence, the
693:
in neighbouring lakes dated to 16,748–16,189, 15,597–12,582 and 12,708–12,567 years Before
Present may originate from Quetrupillán but they have also been attributed to
1654:"Bimodal Holocene flank eruptions at Lanín composite volcano, Southern Volcanic Zone of the Andes: Characterization of their deposits and controls on the vents array"
755:
Annual precipitation exceeds 1,800 millimetres (71 in), with a mean annual temperature of 7.5 °C (45.5 °F). The slopes of Quetrupillán are covered by
554:
melts. A tectonic regime associated with the Liquiñe-Ofqui Fault which prevents magma from simply ascending to the surface may help the magma evolution processes.
1884:
428:
Mocha-Villarrica fault and local structures. There are two lakes on the southern flank, Laguna Azul to the southwest and Laguna Blanca to the southeast.
2573:
1838:
2583:
2568:
1702:
898:
Vilariño, Martín; Ayelén, Ibarra Mendoza (2022). "UN ESCUDO, MUCHAS HISTORIAS: TENSIONES EN TORNO A LA REPRESENTACIÓN SIMBÓLICA DEL VOLCÁN LANÍN".
1734:
1632:
491:
2593:
670:
was formed 1,650 ± 70 years BP, during the largest known eruption of Quetrupillán. This eruption created a 25 kilometres (16 mi) high
547:
374:. In comparison to Villarrica, Quetrupillán has been less active and its eruptions were also smaller than Villarrica's, with no large
2598:
2563:
2553:
1141:"Area changes of glaciers on active volcanoes in Latin America between 1986 and 2015 observed from multi-temporal satellite imagery"
593:
deposits east of the volcano. Several phases of volcanic activity have been inferred from the deposits; most of them feature either
1790:"Tectonic constraints on a magmatic plumbing system: The Quetrupillán Volcanic Complex (39°30′ S, 71°43′ W), Southern Andes, Chile"
985:
743:) fought the other two volcanoes in a century-long conflict; eventually Ruka Pillan was victorious, coinciding with the beginning
61:
1877:
1487:"Synchronisation of sedimentary records using tephra: A postglacial tephrochronological model for the Chilean Lake District"
1338:"Exploring the shallow geothermal resources in the Chilean Southern Volcanic Zone: Insight from the Liquiñe thermal springs"
1735:"The Villarrica-Quetrupillan-Lanin Volcanic Chain: A Review and Probable Significance in the Southern Andes, 39.4°S, Chile"
964:
Schilling, Manuel Enrique; Contreras, María Angélica; Farías, Cristian; Tascón, Gabriela; Partarrieu, Diego (April 2023).
2578:
54:
518:
the main component, and overall more silicic than the rocks erupted by Villarrica and Lanín. Unusually for the region,
2548:
172:
2340:
1909:
798:
706:
675:
2558:
2227:
1870:
1730:
1703:"Estudio aeromagnético de la estructura interna de los volcanes Villarrica y Quetrupillán (Andes del Sur, Chile)"
609:
236:
566:. The first phase of activity involved the formation of calderas and stratovolcanoes; later during the ice ages
2588:
833:
228:
2410:
371:
2430:
857:"De senderos a paisajes: paisajes de las movilidades de una comunidad mapuche en los Andes del sur de Chile"
838:
250:, and is constructed within a field of smaller centres and a larger caldera. It was active during the late
2092:
1851:
1653:
966:"Geoparque Mundial UNESCO Kütralkura: Laboratorio natural para la educación sobre los peligros volcánicos"
351:
332:
328:
232:
143:
1538:"The Space-Time Compression of Indigenous Toponymy: The Case of Mapuche Toponymy in Chilean Norpatagonia"
2082:
2042:
781:
2405:
2350:
1715:
367:
1789:
1337:
203:("blunted", "mutilated"; also known as Ketropillán; the name is sometimes applied to the neighbouring
2445:
2415:
2385:
2345:
2282:
2267:
2157:
2019:
1893:
1801:
1665:
1537:
1498:
1440:
1349:
1301:
1236:
1152:
1139:
Huggel, Christian; Rivera, Andrés; Granados, Hugo Delgado; Paul, Frank; Reinthaler, Johannes (2019).
740:
355:
316:
220:
1747:
1652:
Balbis, C.; Petrinovic, I. A.; Hernando, I. R.; Brod, J. A.; Villegas A., R. J. (1 September 2022).
1614:
459:
has produced two lava flows and is considered to be also part of the Quetrupillán volcanic complex.
28:
2370:
1974:
463:
347:
165:
127:
2503:
2335:
2062:
1825:
1776:
1689:
1565:
1373:
861:
775:
467:
363:
362:
it forms a northwest-southeast alignment of volcanoes, which coincides with the Mocha-Villarrica
900:
Cuadernos del Instituto Nacional de Antropología y Pensamiento Latinoamericano–Series Especiales
343:
282:
231:. Geologically, Quetrupillán is located in a tectonic basement block between the main traces of
212:
965:
938:
2493:
2450:
2425:
2287:
1964:
1929:
1914:
1817:
1681:
1628:
1557:
1365:
1317:
1170:
1007:
915:
880:
490:
rock units. The Villarrica-Quetrupillán volcanic chain forms a geological boundary, since the
320:
286:
278:
2508:
2498:
2420:
2400:
2355:
2232:
2197:
1959:
1934:
1809:
1768:
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1620:
1549:
1516:
1506:
1357:
1309:
1160:
997:
907:
870:
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601:
586:
407:
375:
324:
2325:
2297:
2162:
1984:
1924:
1788:
Simmons, Isla C.; Cortés, Joaquín A.; McGarvie, Dave; Calder, Eliza S. (1 December 2020).
1726:
671:
579:
495:
498:
investigation of the area has found evidence of a possible deep-seated magma reservoir.
1805:
1669:
1502:
1444:
1353:
1305:
1156:
2217:
2142:
786:
621:
487:
452:
412:
108:
685:
was formed 1,380 ± 30 years BP, it is the youngest explosive eruption of Quetrupillán.
2542:
2465:
2460:
2440:
2072:
1944:
1829:
1813:
1780:
1772:
1693:
1677:
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1313:
575:
387:
290:
243:
208:
160:
148:
1511:
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766:
519:
416:
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187:
156:
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1846:
1742:
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770:
702:
527:
456:
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440:
420:
309:
275:
251:
132:
986:"El cambio climático y su influencia en las fluctuaciones del turismo en Chile"
828:
2380:
2212:
2207:
2167:
2137:
2047:
2014:
2009:
1969:
761:
694:
571:
523:
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267:
1821:
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1321:
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1083:
1081:
1068:
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1011:
919:
884:
674:
and deposited about 0.26 cubic kilometres (0.062 cu mi) of rock. A
76:
63:
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2315:
2292:
2257:
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2057:
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551:
539:
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399:
1939:
1521:
1215:
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1186:
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911:
1624:
1589:"Nidificación de Peuquito en los Bosques Templados de la Araucanía Andina"
2518:
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2127:
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2004:
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1994:
1979:
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531:
515:
511:
471:
424:
359:
271:
255:
224:
204:
136:
1165:
1140:
506:
Volcanic rocks at Quetrupillán have a bimodal composition, ranging from
2360:
2277:
2262:
2247:
2152:
2122:
1954:
1949:
722:
605:
563:
479:
395:
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312:
297:
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247:
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690:
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590:
507:
483:
448:
44:
1839:"Tefroestratigrafía postglacial del complejo volcánico Quetrupillán"
705:
composition and the eruptions that generated them have an estimated
638:
was formed 8,680 ± 40 years BP and has a similar composition to the
1862:
2102:
1989:
744:
216:
115:
101:
432:
403:
1866:
1536:
Salazar, Gonzalo; Riquelme Maulén, Wladimir (22 October 2020).
1122:
1120:
1118:
1116:
1114:
1112:
1110:
1108:
1106:
386:
Quetrupillán is a 2,360 metres (7,740 ft) high composite
323:. As the plate subducts, it releases water into the overlying
1039:
1037:
1035:
1033:
1259:
1055:
765:
trees being the most important species; other trees are the
2530:
Note: volcanoes are ordered by latitude from north to south
1457:
1219:
1202:
1190:
1097:
1072:
1024:
562:
Eruptive activity at Quetrupillán commenced before the
447:
anomaly at shallow depth south of the volcano may be a
439:
and maars formed through the interaction of magma with
1414:
1390:
725:
mythology, originally there were just two volcanoes:
850:
848:
2484:
2306:
2033:
1900:
186:
181:
171:
154:
142:
126:
121:
107:
97:
92:
53:
43:
38:
21:
1425:
1423:
1286:
1284:
1282:
1280:
773:. As of 1961, vegetation on Quetrupillán included
1746:. 7th Chilean Geological Congress. Archived from
933:
931:
929:
431:A number of eruption products show traces of ice-
734:
1837:Toloza, Virginia; Moreno, Hugo (October 2015).
1237:"GLACIOVOLCANISM AT VOLCÁN QUETRUPILLÁN, CHILE"
1230:
1228:
1794:Journal of Volcanology and Geothermal Research
1761:Journal of Volcanology and Geothermal Research
1658:Journal of Volcanology and Geothermal Research
1480:
1478:
1294:Journal of Volcanology and Geothermal Research
1878:
1619:. De Gruyter. 1961-12-31. pp. 123, 126.
8:
1469:
1126:
1043:
990:Revista interamericana de ambiente y turismo
578:was emplaced towards the end of glaciation;
308:Off the western coast of South America, the
1613:"Band 4 Allgemeine Vegetationsgeographie".
620:was formed 12,720 ± 40 – 12,690 ± 40 years
604:deposits with varying contents of juvenile
582:formed even later and produced lava flows.
254:; some large eruptions occurred during the
1885:
1871:
1863:
624:(BP) during one rather prolonged eruption.
522:also occurs at the volcano. These contain
18:
1520:
1510:
1164:
1098:Moreno, López-Escobar & Cembrano 1994
1073:Moreno, López-Escobar & Cembrano 1994
1001:
874:
327:and causes it to melt, gives rise to the
33:Quetrupillán with Lanín in the background
342:Quetrupillán lies on the border between
1402:
1271:
809:
534:, with additional microphenocrysts of
339:and dominates the regional tectonics.
823:
821:
819:
817:
815:
813:
678:of 4 has been assigned to this event.
7:
574:were emplaced. Finally, the present
1701:Delgado, Francisco (August 2012).
1342:Journal of Geochemical Exploration
970:Repositorio Institucional INGEMMET
14:
1587:Escobar, Álvaro (December 2022).
939:"Complejo Volcánico Quetrupillán"
1814:10.1016/j.jvolgeores.2020.107101
1773:10.1016/j.jvolgeores.2023.107832
1678:10.1016/j.jvolgeores.2022.107610
1616:Allgemeine Vegetationsgeographie
1314:10.1016/j.jvolgeores.2018.04.020
855:Huiliñir-Curío, Viviana (2018).
631:was formed 10,240 ± 40 years BP.
27:
1512:10.1016/j.quascirev.2016.02.015
1235:McGarvie, Dave (October 2014).
1003:10.4067/S0718-235X2022000200118
876:10.4067/S0717-73562018005001301
663:was formed 2,060 ± 30 years BP.
656:was formed 2,930 ± 30 years BP.
649:was formed 3,800 ± 30 years BP.
266:The volcano is situated in the
486:rocks. These are plutonic and
1:
2574:Volcanoes of Araucanía Region
1554:10.1080/00167428.2020.1839898
589:, which have formed flow and
2584:Mountains of Los Ríos Region
2569:Volcanoes of Los Ríos Region
1850:(in Spanish). Archived from
1714:(in Spanish). Archived from
1602:. Fundación Mar Adentro: 40.
1362:10.1016/j.gexplo.2020.106611
242:The volcano consists of one
49:2,360 m (7,740 ft)
2594:Pleistocene stratovolcanoes
697:. All these tephras are of
2615:
1491:Quaternary Science Reviews
1433:AGU Fall Meeting Abstracts
799:List of volcanoes in Chile
707:volcanic explosivity index
676:volcanic explosivity index
548:Fractional crystallization
482:Trápatrapa formations and
474:Panguipulli, the possibly
2527:
721:According to a tale from
585:Quetrupillán has erupted
394:cover; the existence of
335:has developed within the
237:Reigolil-Pirihueico Fault
219:. It is situated between
26:
2599:Holocene stratovolcanoes
2564:Villarrica National Park
2554:Stratovolcanoes of Chile
1470:Toloza & Moreno 2015
1127:Toloza & Moreno 2015
1044:Toloza & Moreno 2015
834:Global Volcanism Program
229:Villarrica National Park
1733:; Cembrano, J. (1994).
839:Smithsonian Institution
735:
661:Trancas Negras sequence
612:and ash fall deposits.
494:crops out south of it.
415:south of Quetrupillán.
378:found at Quetrupillán.
2307:Southern Volcanic Zone
2093:Andagua volcanic field
1901:Northern Volcanic Zone
912:10.5281/zenodo.7694088
751:Climate and vegetation
352:Southern Volcanic Zone
329:Southern Volcanic Zone
2485:Austral Volcanic Zone
2411:Puyehue-Cordón Caulle
2083:Huambo volcanic field
2034:Central Volcanic Zone
1857:on November 20, 2021.
1753:on December 10, 2017.
1721:on November 25, 2021.
1625:10.1515/9783111616728
1145:Journal of Glaciology
782:Nothofagus antarctica
550:of basalts generated
470:of Quetrupillán: The
372:Puyehue-Cordón Caulle
296:and are an important
262:Geology and geography
194:Palguín - Laguna Azul
2020:Licto volcanic field
785:forests, as well as
492:Patagonian Batholith
317:South American Plate
2579:South Volcanic Zone
1806:2020JVGR..40707101S
1670:2022JVGR..42907610B
1542:Geographical Review
1503:2016QSRv..137..234F
1472:, pp. 574–575.
1458:Simmons et al. 2020
1445:2015AGUFM.V43B3122B
1354:2020JCExp.21806611D
1306:2018JVGR..357..163B
1220:Simmons et al. 2020
1203:Simmons et al. 2020
1191:Simmons et al. 2020
1166:10.1017/jog.2019.30
1157:2019JGlac..65..542R
1025:Simmons et al. 2020
733:. Then the volcano
689:In addition, three
654:Correntoso sequence
478:Currarehue and the
333:Liquiñe-Ofqui Fault
233:Liquiñe-Ofqui Fault
166:South Volcanic Zone
73: /
2549:Mountains of Chile
2406:Carrán-Los Venados
2351:Nevados de Chillán
2336:Descabezado Grande
1260:Balbis et al. 2022
1056:Balbis et al. 2022
789:-like vegetation.
776:Araucaria araucana
640:Avutardas sequence
451:associated with a
368:Nevados de Chillán
364:transcurrent fault
235:(to the west) and
227:volcanoes, within
39:Highest point
2536:
2535:
2346:Nevado de Longaví
2288:Cueros de Purulla
2268:Cordón del Azufre
1930:Nevado del Tolima
1731:López-Escobar, L.
1634:978-3-11-161672-8
1415:Pavez et al. 2023
1391:Pavez et al. 2023
757:temperate forests
636:Trancura sequence
408:pyroclastic cones
376:pyroclastic flows
321:Peru-Chile Trench
198:
197:
16:Mountain in Chile
2606:
2559:Active volcanoes
2531:
2401:Mocho-Choshuenco
1935:Nevado del Huila
1894:Andean volcanoes
1887:
1880:
1873:
1864:
1858:
1856:
1843:
1833:
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1016:
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1005:
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973:
961:
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954:
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950:
935:
924:
923:
895:
889:
888:
878:
862:Chungará (Arica)
852:
843:
842:
825:
738:
602:pyroclastic flow
558:Eruptive history
462:Three different
390:and a shrinking
354:. Together with
348:Araucanía Region
190:
111:
88:
87:
85:
84:
83:
78:
74:
71:
70:
69:
66:
31:
19:
2614:
2613:
2609:
2608:
2607:
2605:
2604:
2603:
2589:VEI-4 volcanoes
2539:
2538:
2537:
2532:
2529:
2523:
2486:
2480:
2308:
2302:
2298:Ojos del Salado
2228:Aguas Calientes
2035:
2029:
1925:Nevado del Ruiz
1902:
1896:
1891:
1861:
1854:
1841:
1836:
1787:
1757:
1750:
1737:
1725:
1718:
1705:
1700:
1651:
1647:
1642:
1635:
1612:
1611:
1607:
1591:
1586:
1585:
1581:
1535:
1534:
1530:
1522:1854/LU-7144061
1484:
1483:
1476:
1468:
1464:
1456:
1452:
1429:
1428:
1421:
1413:
1409:
1401:
1397:
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1329:
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1234:
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1209:
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1138:
1137:
1133:
1125:
1104:
1096:
1079:
1071:
1062:
1054:
1050:
1042:
1031:
1027:, pp. 1–2.
1023:
1019:
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981:
977:
963:
962:
958:
948:
946:
937:
936:
927:
897:
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811:
807:
795:
753:
719:
672:eruption column
668:Puesco sequence
618:Moraga sequence
580:parasitic vents
560:
504:
496:Magnetotelluric
384:
344:Los Ríos Region
306:
264:
239:(to the east).
213:Los Ríos Region
207:volcano.) is a
188:
109:
81:
79:
75:
72:
67:
64:
62:
60:
59:
34:
17:
12:
11:
5:
2612:
2610:
2602:
2601:
2596:
2591:
2586:
2581:
2576:
2571:
2566:
2561:
2556:
2551:
2541:
2540:
2534:
2533:
2528:
2525:
2524:
2522:
2521:
2516:
2511:
2506:
2501:
2496:
2490:
2488:
2482:
2481:
2479:
2478:
2473:
2468:
2463:
2458:
2453:
2448:
2443:
2438:
2433:
2428:
2423:
2418:
2413:
2408:
2403:
2398:
2393:
2388:
2383:
2378:
2373:
2368:
2363:
2358:
2353:
2348:
2343:
2338:
2333:
2328:
2323:
2318:
2312:
2310:
2304:
2303:
2301:
2300:
2295:
2290:
2285:
2280:
2275:
2270:
2265:
2260:
2255:
2250:
2245:
2240:
2235:
2230:
2225:
2220:
2218:Purico complex
2215:
2210:
2205:
2200:
2195:
2190:
2185:
2180:
2175:
2170:
2165:
2160:
2155:
2150:
2145:
2140:
2135:
2130:
2125:
2120:
2115:
2110:
2105:
2100:
2095:
2090:
2085:
2080:
2075:
2070:
2065:
2060:
2055:
2050:
2045:
2039:
2037:
2031:
2030:
2028:
2027:
2022:
2017:
2012:
2007:
2002:
1997:
1992:
1987:
1982:
1977:
1972:
1967:
1962:
1957:
1952:
1947:
1942:
1937:
1932:
1927:
1922:
1917:
1912:
1906:
1904:
1898:
1897:
1892:
1890:
1889:
1882:
1875:
1867:
1860:
1859:
1834:
1785:
1755:
1723:
1698:
1648:
1646:
1643:
1641:
1640:
1633:
1605:
1598:(in Spanish).
1579:
1528:
1474:
1462:
1450:
1419:
1407:
1405:, p. 624.
1395:
1383:
1327:
1276:
1274:, p. 625.
1264:
1252:
1241:gsa.confex.com
1224:
1207:
1195:
1180:
1131:
1129:, p. 575.
1102:
1100:, p. 340.
1077:
1075:, p. 339.
1060:
1048:
1046:, p. 574.
1029:
1017:
996:(2): 118–136.
975:
956:
925:
902:(in Spanish).
890:
869:(3): 487–499.
844:
829:"Quetrupillan"
808:
806:
803:
802:
801:
794:
791:
752:
749:
718:
715:
687:
686:
683:Carén sequence
679:
664:
657:
650:
647:Carén sequence
643:
632:
629:Puala sequence
625:
622:Before Present
559:
556:
503:
500:
488:volcaniclastic
453:resurgent dome
435:interactions.
413:volcanic field
383:
380:
305:
302:
279:municipalities
263:
260:
246:with a summit
196:
195:
192:
184:
183:
179:
178:
175:
169:
168:
163:
152:
151:
146:
140:
139:
130:
124:
123:
119:
118:
113:
105:
104:
99:
95:
94:
90:
89:
57:
51:
50:
47:
41:
40:
36:
35:
32:
24:
23:
15:
13:
10:
9:
6:
4:
3:
2:
2611:
2600:
2597:
2595:
2592:
2590:
2587:
2585:
2582:
2580:
2577:
2575:
2572:
2570:
2567:
2565:
2562:
2560:
2557:
2555:
2552:
2550:
2547:
2546:
2544:
2526:
2520:
2517:
2515:
2512:
2510:
2507:
2505:
2502:
2500:
2497:
2495:
2492:
2491:
2489:
2483:
2477:
2474:
2472:
2469:
2467:
2464:
2462:
2459:
2457:
2454:
2452:
2449:
2447:
2444:
2442:
2441:Michinmahuida
2439:
2437:
2434:
2432:
2429:
2427:
2424:
2422:
2419:
2417:
2414:
2412:
2409:
2407:
2404:
2402:
2399:
2397:
2394:
2392:
2389:
2387:
2384:
2382:
2379:
2377:
2374:
2372:
2369:
2367:
2364:
2362:
2359:
2357:
2354:
2352:
2349:
2347:
2344:
2342:
2339:
2337:
2334:
2332:
2329:
2327:
2324:
2322:
2319:
2317:
2314:
2313:
2311:
2305:
2299:
2296:
2294:
2291:
2289:
2286:
2284:
2283:San Francisco
2281:
2279:
2276:
2274:
2271:
2269:
2266:
2264:
2261:
2259:
2256:
2254:
2251:
2249:
2246:
2244:
2241:
2239:
2236:
2234:
2231:
2229:
2226:
2224:
2221:
2219:
2216:
2214:
2211:
2209:
2206:
2204:
2201:
2199:
2196:
2194:
2193:Aucanquilcha
2191:
2189:
2186:
2184:
2181:
2179:
2176:
2174:
2171:
2169:
2166:
2164:
2161:
2159:
2156:
2154:
2151:
2149:
2146:
2144:
2141:
2139:
2136:
2134:
2131:
2129:
2126:
2124:
2121:
2119:
2116:
2114:
2111:
2109:
2106:
2104:
2101:
2099:
2096:
2094:
2091:
2089:
2086:
2084:
2081:
2079:
2076:
2074:
2073:Hualca Hualca
2071:
2069:
2066:
2064:
2061:
2059:
2056:
2054:
2051:
2049:
2046:
2044:
2041:
2040:
2038:
2032:
2026:
2023:
2021:
2018:
2016:
2013:
2011:
2008:
2006:
2003:
2001:
1998:
1996:
1993:
1991:
1988:
1986:
1983:
1981:
1978:
1976:
1973:
1971:
1968:
1966:
1963:
1961:
1958:
1956:
1953:
1951:
1948:
1946:
1943:
1941:
1938:
1936:
1933:
1931:
1928:
1926:
1923:
1921:
1918:
1916:
1913:
1911:
1908:
1907:
1905:
1903:(6° N – 3° S)
1899:
1895:
1888:
1883:
1881:
1876:
1874:
1869:
1868:
1865:
1853:
1849:
1848:
1840:
1835:
1831:
1827:
1823:
1819:
1815:
1811:
1807:
1803:
1799:
1795:
1791:
1786:
1782:
1778:
1774:
1770:
1766:
1762:
1756:
1749:
1745:
1744:
1736:
1732:
1728:
1724:
1717:
1713:
1712:
1704:
1699:
1695:
1691:
1687:
1683:
1679:
1675:
1671:
1667:
1663:
1659:
1655:
1650:
1649:
1644:
1636:
1630:
1626:
1622:
1618:
1617:
1609:
1606:
1601:
1597:
1590:
1583:
1580:
1575:
1571:
1567:
1563:
1559:
1555:
1551:
1547:
1543:
1539:
1532:
1529:
1523:
1518:
1513:
1508:
1504:
1500:
1496:
1492:
1488:
1481:
1479:
1475:
1471:
1466:
1463:
1460:, p. 16.
1459:
1454:
1451:
1446:
1442:
1439:: V43B–3122.
1438:
1434:
1426:
1424:
1420:
1416:
1411:
1408:
1404:
1399:
1396:
1392:
1387:
1384:
1379:
1375:
1371:
1367:
1363:
1359:
1355:
1351:
1347:
1343:
1339:
1331:
1328:
1323:
1319:
1315:
1311:
1307:
1303:
1299:
1295:
1287:
1285:
1283:
1281:
1277:
1273:
1268:
1265:
1262:, p. 15.
1261:
1256:
1253:
1242:
1238:
1231:
1229:
1225:
1221:
1216:
1214:
1212:
1208:
1205:, p. 13.
1204:
1199:
1196:
1192:
1187:
1185:
1181:
1176:
1172:
1167:
1162:
1158:
1154:
1150:
1146:
1142:
1135:
1132:
1128:
1123:
1121:
1119:
1117:
1115:
1113:
1111:
1109:
1107:
1103:
1099:
1094:
1092:
1090:
1088:
1086:
1084:
1082:
1078:
1074:
1069:
1067:
1065:
1061:
1057:
1052:
1049:
1045:
1040:
1038:
1036:
1034:
1030:
1026:
1021:
1018:
1013:
1009:
1004:
999:
995:
991:
987:
979:
976:
971:
967:
960:
957:
944:
940:
934:
932:
930:
926:
921:
917:
913:
909:
905:
901:
894:
891:
886:
882:
877:
872:
868:
864:
863:
858:
851:
849:
845:
840:
836:
835:
830:
824:
822:
820:
818:
816:
814:
810:
804:
800:
797:
796:
792:
790:
788:
784:
783:
778:
777:
772:
768:
764:
763:
758:
750:
748:
746:
742:
737:
732:
728:
724:
716:
714:
710:
708:
704:
700:
696:
692:
684:
680:
677:
673:
669:
665:
662:
658:
655:
651:
648:
644:
641:
637:
633:
630:
626:
623:
619:
615:
614:
613:
611:
607:
603:
600:
596:
592:
588:
583:
581:
577:
576:stratovolcano
573:
569:
565:
557:
555:
553:
549:
543:
541:
537:
533:
529:
525:
521:
517:
513:
509:
501:
499:
497:
493:
489:
485:
481:
477:
473:
469:
465:
460:
458:
454:
450:
446:
442:
438:
434:
429:
426:
422:
418:
417:Fissure vents
414:
409:
405:
401:
397:
393:
389:
388:stratovolcano
381:
379:
377:
373:
369:
365:
361:
357:
353:
349:
345:
340:
338:
334:
330:
326:
322:
318:
314:
311:
303:
301:
300:destination.
299:
295:
292:
288:
284:
280:
277:
273:
269:
261:
259:
257:
253:
249:
245:
244:stratovolcano
240:
238:
234:
230:
226:
222:
218:
214:
210:
209:stratovolcano
206:
202:
193:
191:
189:Easiest route
185:
180:
176:
174:
173:Last eruption
170:
167:
164:
162:
158:
153:
150:
149:Stratovolcano
147:
145:
144:Mountain type
141:
138:
134:
131:
129:
125:
120:
117:
114:
112:
106:
103:
100:
96:
91:
86:
77:39.5°S 71.7°W
58:
56:
52:
48:
46:
42:
37:
30:
25:
20:
2391:Quetrupillán
2390:
2253:Llullaillaco
2118:Huaynaputina
1852:the original
1845:
1797:
1793:
1764:
1760:
1748:the original
1741:
1716:the original
1709:
1661:
1657:
1615:
1608:
1599:
1596:La Chiricoca
1595:
1582:
1574:ResearchGate
1572:– via
1545:
1541:
1531:
1494:
1490:
1465:
1453:
1436:
1432:
1417:, p. 3.
1410:
1403:Delgado 2012
1398:
1393:, p. 4.
1386:
1345:
1341:
1330:
1297:
1293:
1272:Delgado 2012
1267:
1255:
1244:. Retrieved
1240:
1222:, p. 2.
1198:
1193:, p. 3.
1148:
1144:
1134:
1058:, p. 2.
1051:
1020:
993:
989:
978:
969:
959:
947:. Retrieved
945:(in Spanish)
942:
903:
899:
893:
866:
860:
832:
780:
774:
771:maniú hembra
760:
754:
720:
711:
688:
682:
667:
660:
653:
646:
639:
635:
628:
617:
587:pyroclastics
584:
561:
544:
520:trachydacite
505:
466:make up the
461:
430:
385:
341:
337:volcanic arc
315:beneath the
307:
265:
241:
201:Quetrupillán
200:
199:
110:Parent range
82:-39.5; -71.7
22:Quetrupillán
2487:(49°–55° S)
2471:Mate Grande
2321:Tupungatito
2309:(33°–46° S)
2188:Olca-Paruma
2183:Irruputuncu
2173:Tata Sabaya
2113:Pichu Pichu
2043:Quimsachata
2036:(14°–27° S)
1920:Cerro Bravo
1847:SERNAGEOMIN
1743:SERNAGEOMIN
1711:SERNAGEOMIN
1300:: 163–176.
943:SERNAGEOMIN
736:Ruka Pillan
703:rhyodacitic
599:scoriaceous
572:ignimbrites
528:plagioclase
524:phenocrysts
502:Composition
457:scoria cone
455:. Huililco
445:geomagnetic
441:groundwater
421:Pleistocene
310:Nazca Plate
276:Panguipulli
252:Pleistocene
211:located in
133:Pleistocene
128:Age of rock
80: /
55:Coordinates
2543:Categories
2431:Hornopirén
2416:Casablanca
2386:Villarrica
2381:Sollipulli
2341:Cerro Azul
2213:Licancabur
2208:Sairecabur
2168:Guallatiri
2158:Parinacota
2138:Purupuruni
2048:Auquihuato
2015:Tungurahua
2010:Chimborazo
1970:Reventador
1945:Doña Juana
1800:: 107101.
1767:: 107832.
1727:Moreno, R.
1664:: 107610.
1348:: 106611.
1246:2017-06-13
1151:(252): 9.
949:22 October
906:(1): 429.
805:References
762:Nothofagus
747:conquest.
741:Villarrica
727:Choshuenco
695:Sollipulli
568:lava flows
476:Cretaceous
464:formations
437:Tuff rings
400:lava domes
356:Villarrica
291:Kütralkura
268:Curarrehue
221:Villarrica
2451:Corcovado
2371:Lonquimay
2331:Calabozos
2316:Tupungato
2293:Incahuasi
2258:Lastarria
2238:Chiliques
2078:Sabancaya
2058:Sara Sara
1975:Pichincha
1910:Paipa-Iza
1830:228986088
1822:0377-0273
1781:259828474
1694:249840260
1686:0377-0273
1570:226336183
1562:0016-7428
1548:(5): 21.
1378:224938471
1370:0375-6742
1322:0377-0273
1175:0022-1430
1012:0718-235X
920:2362-1958
885:0717-7356
717:Mythology
699:rhyolitic
595:pumiceous
552:trachytic
540:magnetite
350:, in the
258:as well.
177:June 1872
155:Volcanic
93:Geography
45:Elevation
2519:Fueguino
2504:Aguilera
2456:Mentolat
2366:Callaqui
2203:Zapaleri
2133:Yucamane
2128:Tutupaca
2098:Chachani
2068:Coropuna
2063:Solimana
2005:Quilotoa
2000:Cotopaxi
1995:Illiniza
1980:Antisana
793:See also
769:and the
564:ice ages
536:ilmenite
532:pyroxene
516:trachyte
512:andesite
484:plutonic
472:Triassic
468:basement
425:Holocene
396:calderas
313:subducts
304:Regional
287:Valdivia
256:Holocene
182:Climbing
137:Holocene
98:Location
2494:Lautaro
2446:Chaitén
2426:Calbuco
2361:Copahue
2278:Peinado
2263:Lazufre
2248:Socompa
2153:Taapaca
2123:Ticsani
1965:Cayambe
1955:Azufral
1950:Galeras
1915:Romeral
1802:Bibcode
1666:Bibcode
1645:Sources
1499:Bibcode
1497:: 238.
1441:Bibcode
1350:Bibcode
1302:Bibcode
1153:Bibcode
759:, with
745:Spanish
723:Mapuche
691:tephras
610:lithics
606:lapilli
480:Miocene
392:glacier
319:in the
298:tourism
294:geopark
281:of the
248:caldera
122:Geology
68:71°42′W
65:39°30′S
2514:Burney
2509:Reclus
2499:Viedma
2476:Hudson
2436:Huequi
2421:Osorno
2376:Llaima
2356:Antuco
2243:Aracar
2233:Lascar
2223:Pacana
2198:Azufre
2178:Isluga
2148:Tacora
2143:Casiri
2108:Ubinas
2088:Ampato
2053:Firura
2025:Sangay
1960:Chiles
1940:Puracé
1828:
1820:
1779:
1692:
1684:
1631:
1568:
1560:
1376:
1368:
1320:
1173:
1010:
972:: 401.
918:
883:
709:of 3.
591:pumice
508:basalt
449:pluton
325:mantle
283:Cautín
2396:Lanín
2326:Maipo
2273:Galán
2163:Lauca
2103:Misti
1990:Soche
1985:Aliso
1855:(PDF)
1842:(PDF)
1826:S2CID
1777:S2CID
1751:(PDF)
1738:(PDF)
1719:(PDF)
1706:(PDF)
1690:S2CID
1592:(PDF)
1566:S2CID
1374:S2CID
731:Lanín
514:with
404:maars
382:Local
360:Lanín
272:Pucón
225:Lanín
217:Chile
205:Lanín
116:Andes
102:Chile
2466:Macá
1818:ISSN
1682:ISSN
1629:ISBN
1558:ISSN
1366:ISSN
1318:ISSN
1171:ISSN
1008:ISSN
951:2022
916:ISSN
881:ISSN
787:puna
779:and
767:tepa
729:and
681:The
666:The
659:The
652:The
645:The
634:The
627:The
616:The
570:and
538:and
530:and
443:. A
433:lava
406:and
370:and
358:and
346:and
285:and
274:and
223:and
161:belt
2461:Cay
1810:doi
1798:407
1769:doi
1765:439
1674:doi
1662:429
1621:doi
1550:doi
1546:112
1517:hdl
1507:doi
1495:137
1358:doi
1346:218
1310:doi
1298:357
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