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Journal articles on the topic 'Cordillera de la Sal (Chile)'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

De Waele, Jo, Vincenzo Picotti, Mario L. V. Martina, George Brook, Linhai Yang, and Paolo Forti. "Holocene evolution of halite caves in the Cordillera de la Sal (Central Atacama, Chile) in different climate conditions." Geomorphology 370 (December 2020): 107398. http://dx.doi.org/10.1016/j.geomorph.2020.107398.

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2

Sesiano, Jean. "Evolution actuelle des phénomènes karstiques dans la Cordillera de la Sal (Atacama, Nord Chili)." Karstologia : revue de karstologie et de spéléologie physique 47, no. 1 (2006): 49–54. http://dx.doi.org/10.3406/karst.2006.2577.

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3

Pisani, Luca, and Jo De Waele. "Candidate cave entrances in a planetary analogue evaporite karst (Cordillera de la Sal, Chile): A remote sensing approach and ground-truth reconnaissance." Geomorphology 389 (September 2021): 107851. http://dx.doi.org/10.1016/j.geomorph.2021.107851.

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4

Rubilar, Juan, Fernando Martínez, César Arriagada, Juan Becerra, and Sebastián Bascuñán. "Structure of the Cordillera de la Sal: A key tectonic element for the Oligocene-Neogene evolution of the Salar de Atacama basin, Central Andes, northern Chile." Journal of South American Earth Sciences 87 (November 2018): 200–210. http://dx.doi.org/10.1016/j.jsames.2017.11.013.

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5

Suarez, M., M. Herve, and A. Puig. "Cretaceous diapiric plutonism in the southern cordillera, Chile." Geological Magazine 124, no. 6 (1987): 569–75. http://dx.doi.org/10.1017/s0016756800017398.

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AbstractThe Castores and probably the Santa Rosa plutons of north-west Isla Navarino, southern Chile, have been emplaced by in situ diapirism into metasedimentary rocks of the Upper Jurassic (?)–Lower Cretaceous Yaghan Formation. For the former, this model is consistent with the concentric foliation paralleling the margin of the pluton and the foliation and stratification planes in the metamorphic aureole. Only the southern part of the Santa Rosa Pluton is preserved, and it has some structures similar to those of the Castores Pluton, which can also be interpreted as produced by an inflating di

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6

Kuschel, Katherina, Francisco Cotapos, and Sebastián Hercovich. "Renew Your Wardrobe: ‘Climbing the Cordillera’." South Asian Journal of Business and Management Cases 5, no. 1 (2016): 13–20. http://dx.doi.org/10.1177/2277977916634220.

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Cecilia Membrado is the founder of a marketplace platform for buying and selling second-hand fashionable clothes, that was established in Argentina in 2014. Cecilia needs to take her business to a global scale, starting with opening operations in Chile. The case details all the initiatives taken by the entrepreneur in her start-up and to resolve the issues on her journey to achieve success to the case is largely developed from primary sources.

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7

Gacitúa, Guisella, Christoph Schneider, Jorge Arigony, Inti González, Ricardo Jaña, and Gino Casassa. "First ice thickness measurements in Tierra del Fuego at Schiaparelli Glacier, Chile." Earth System Science Data 13, no. 2 (2021): 231–36. http://dx.doi.org/10.5194/essd-13-231-2021.

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Abstract. Cordillera Darwin in Tierra del Fuego (Chile) remains one of the least studied glaciated regions in the world. However, this region being one of very few terrestrial sites at this latitude in the Southern Hemisphere has the potential to provide key information on the effect of climate variability and climate change on the cryosphere at sub-polar mid-latitudes of the Southern Hemisphere. Schiaparelli Glacier is located at the northern side of the Cordillera Darwin draining the north side of Monte Sarmiento (2187 m a.s.l.). Despite being one of the largest glaciers in the Cordillera Da

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8

Hall, Brenda. "Deglaciation of Cordillera Darwin, southern Chile, during the last termination." Quaternary International 279-280 (November 2012): 185. http://dx.doi.org/10.1016/j.quaint.2012.08.299.

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9

Breitkreuz, Christoph, and Heinrich Bahlburg. "Palaeozoic flysch series in the Coastal Cordillera of Northern Chile." Geologische Rundschau 74, no. 3 (1985): 565–72. http://dx.doi.org/10.1007/bf01821212.

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10

Hartley, Adrian J., Anne E. Mather, Elizabeth Jolley, and Peter Turner. "Climatic controls on alluvial-fan activity, Coastal Cordillera, northern Chile." Geological Society, London, Special Publications 251, no. 1 (2005): 95–116. http://dx.doi.org/10.1144/gsl.sp.2005.251.01.08.

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11

Eliash D., Humberto. "Encuentro Internacional sobre Arquitectura y Urbanismo en América :universidades UNICAMP y PUC de Campinas, Sao Paulo, Brasil reflexiones desde Chile sobre los 25 años de Seminarios de Arquitectura Latinoamericana." Revista de Arquitectura 16, no. 21 (2010): 8. http://dx.doi.org/10.5354/0719-5427.2010.27878.

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Los Seminarios de Arquitectura Latinoamericana (SAL) tuvieron –desde su creación en Buenos Aires en 1985– un destacado rol en la cultura arquitectónica latinoamericana en las décadas de los ’80 y ’90. En torno a ellos se articuló el encuentro entre el mundo teórico y el de la práctica profesional, entre los arquitectos dedicados a la enseñanza, la crítica y la historia. Chile participó activamente de estos encuentros con un balance positivo en sus primeros años. Sin embargo la influencia de los SAL ha decaído. Este texto plantea tres reflexiones para intentar explicar la pérdida de influencia

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12

Le Quesne, Carlos, David W. Stahle, Malcolm K. Cleaveland, Matthew D. Therrell, Juan Carlos Aravena, and Jonathan Barichivich. "Ancient Austrocedrus Tree-Ring Chronologies Used to Reconstruct Central Chile Precipitation Variability from a.d. 1200 to 2000." Journal of Climate 19, no. 22 (2006): 5731–44. http://dx.doi.org/10.1175/jcli3935.1.

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Abstract An expanded network of moisture-sensitive tree-ring chronologies has been developed for central Chile from long-lived cypress trees in the Andean Cordillera. A regional ring width chronology of cypress sites has been used to develop well-calibrated and verified estimates of June–December precipitation totals for central Chile extending from a.d. 1200 to 2000. These reconstructions are confirmed in part by historical references to drought in the seventeenth and eighteenth centuries and by nineteenth-century observations on the position of the Río Cipreses glacier. Analyses of the retur

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13

Litton, Creighton M., and Rómulo Santelices. "Early post-fire succession in a Nothofagus glauca forest in the Coastal Cordillera of south-central Chile." International Journal of Wildland Fire 11, no. 2 (2002): 115. http://dx.doi.org/10.1071/wf02039.

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The temperate deciduous species Nothofagus glauca (Phil.) Krasser exhibits characteristics commonly found in fire-adapted vegetation, yet the role of fire in the evolutionary history of the vegetation in south-central Chile has not been well investigated. We examined the effects of a wildfire on early succession in a Nothofagus glauca forest in the Coastal Cordillera of south-central Chile by comparing data from a burned forest to the vegetation in an adjacent, unburned stand.

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14

Barrett, Bradford S., RenéD Garreaud, and Mark Falvey. "Effect of the Andes Cordillera on Precipitation from a Midlatitude Cold Front." Monthly Weather Review 137, no. 9 (2009): 3092–109. http://dx.doi.org/10.1175/2009mwr2881.1.

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Abstract The effects of the Andes Cordillera, the major mountain range in South America, on precipitation patterns of baroclinic systems approaching from the southeast Pacific remain largely unstudied. This study focuses on a case in late May 2008 when an upper-level trough and surface cold front produced widespread precipitation in central Chile. The primary goal was to analyze the physical mechanisms responsible for the structure and evolution of the precipitation. Weather Research and Forecasting (WRF) model simulations indicate that as an upper-level trough approached central Chile, midtro

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15

Bahr, Jurgen. "Agriculture, Copper Mining, and Migration in the Andean Cordillera of Northern Chile." Mountain Research and Development 5, no. 3 (1985): 279. http://dx.doi.org/10.2307/3673359.

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16

Troncoso, Alejandro, and Rafael Herbst. "The Triassic flora of Cajón Troncoso, Cordillera del Maule, 7th Region, Chile." Revista del Museo Argentino de Ciencias Naturales 2 (2000): 137–44. http://dx.doi.org/10.22179/revmacn.2.149.

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17

Kuylenstierna, J. L., G. C. Rosqvist, and P. Holmlund. "Late-Holocene glacier variations in the Cordillera Darwin, Tierra del Fuego, Chile." Holocene 6, no. 3 (1996): 353–58. http://dx.doi.org/10.1177/095968369600600310.

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18

Giribas, C., G. Paredes, and A. Riquelme. "RECOVERING VALPARAÍSO'S URBAN ELEVATORS: THE RESTORATION OF THE CORDILLERA FUNICULAR." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLIV-M-1-2020 (July 24, 2020): 535–42. http://dx.doi.org/10.5194/isprs-archives-xliv-m-1-2020-535-2020.

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Abstract. During the 19th century, the port of Valparaíso was the place in Chile with the closest links to the rest of the world, leading to strong social, cultural and technological transformations in the city. The arrival of the industrial revolution together with foreign influence led to the apparition of machinism; which along with the need to connect the lower area of the city with the hills led to the construction of several urban elevators. More than thirty elevators functioned throughout Valparaíso during the 20th century, out of which less than a half remained operational at the begin

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19

Hall, B. L., G. Denton, T. Lowell, G. R. M. Bromley, and A. E. Putnam. "Retreat of the Cordillera Darwin icefield during Termination I." Cuadernos de Investigación Geográfica 43, no. 2 (2017): 751. http://dx.doi.org/10.18172/cig.3158.

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During the last glaciation, the Cordillera Darwin icefield expanded northward toward the Straits of Magellan, eastward across Isla Grande de Tierra del Fuego and through Canal Beagle, and south and west across the numerous islands of southernmost Chile. Deglaciation commenced at ~18 ka during Termination I. Alpine glaciers in the Fuegian Andes also likely retreated at that time. Radiocarbon ages from the interior regions of Cordillera Darwin suggest ice in at least some locations had retreated close to its present-day limit as early as ~16.5 ka. The most likely cause for such rapid ice retreat

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20

WILSON, RYAN, SEBASTIAN H. MERNILD, JEPPE K. MALMROS, CLAUDIO BRAVO, and DANIELA CARRIÓN. "Surface velocity fluctuations for Glaciar Universidad, central Chile, between 1967 and 2015." Journal of Glaciology 62, no. 235 (2016): 847–60. http://dx.doi.org/10.1017/jog.2016.73.

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ABSTRACTFor the Andes Cordillera, where observed mass-balance records are sparse, long-term glacier velocity measurements potentially represent a useful tool for assessing glacier health. Utilising manual and automatic feature-tracking techniques applied to Corona, Landsat and ASTER satellite imagery, this paper presents surface velocity fluctuations for Glaciar Universidad between 1967 and 1969, and 1985 and 2015, the longest such time series available for the Andes Cordillera, outside Patagonia. This time series reveals an increase in the surface velocities of the main glacier trunk between

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21

Riccardi, Alberto C. "Callovian and Oxfordian (Jurassic) teuthids (Coleoidea, Cephalopoda) from Chile." Journal of Paleontology 90, no. 5 (2016): 910–22. http://dx.doi.org/10.1017/jpa.2016.110.

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AbstractColeoid specimens from the Jurassic of northern Chile are included in two different species ofTrachyteuthis, i.e.,T. covacevichiFuchs and Schultze, 2008 andT. chilensisn. sp., and in a new genus and a new species,Pseudoteudopsis perezin. gen. n. sp. The specimens described and figured are from two different areas in northern Chile. Those referred toPseudoteudopsis perezin. gen. n. sp. came from a locality north of Calama and are associated with ammonites indicating the lower Callovian uppermostbodenbenderito lowermostproximumzones (≈gracilisStandard Zone) of the Andean ammonite zonatio

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22

Bonilla Rivera, Pablo Enrique. "Investigación fitoquímica, farmacológica y de toxicidad DL₅₀ de Ephedra Americana Pinco-Pinco." Ciencia e Investigación 2, no. 1 (1999): 27–43. http://dx.doi.org/10.15381/ci.v2i1.4404.

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Una yerba que crece a lo largo de la Cordillera de los Andes, denominada por los nativos Pinco-Pinco, y de amplio uso medicinal en la zona andina del Perú, en la altiplanicie de Bolivia y a lo largo de la cordillera andina de Argentina y Chile, cuyo nombre científico es Ephedra americana, es especie vegetal objeto de la presente investigación.En nuestro país esta especie crece abundantemente en el departamento de Arequipa, en el balneario de Jesús, en el camino a la Laguna de Salinas en faldas del nevado Pichu-Pichu.También crece en forma abundante en el Cusco. La muestra vegetal del presente

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23

Naranjo, J. A., A. Puig, and M. Suárez. "A note on Lower Jurassic magmatism in the Coastal Cordillera of Atacama, Chile." Geological Magazine 123, no. 6 (1986): 699–702. http://dx.doi.org/10.1017/s0016756800024213.

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AbstractRadiometric dates on specimens of plutons of the Coastal Cordillera of Atacama span the period 300–110 Ma. A group of dates cluster around 190 Ma and evidence is presented which strongly suggests that they represent near crystallization ages. The geographic distribution of these plutons, adjacent to Liassic tuffs and lavas (Pan de Azúcar and Posada de los Hidalgo formations), suggests a genetic relationship between them, and that the plutons were the roots of the Lower Jurassic volcanic chain. The location of these granitoids to the west of the Liassic volcanic rocks, favours a previou

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24

Holmlund, Per, and Humberto Fuenzalida. "Anomalous glacier responses to 20th century climatic changes in Darwin Cordillera, southern Chile." Journal of Glaciology 41, no. 139 (1995): 465–73. http://dx.doi.org/10.1017/s0022143000034808.

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AbstractThere is an asymmetric pattern response of glaciers in Darwin Cordillera (54–55° S, 69–71° W) to the climate of the 20th century. This asymmetry is suggested here as a cause of an increased wind activity which has a pronounced orographic effect. Although climatic records for the last 50 years show a warming trend, as well as no trend in precipitation in the area, some glaciers are advancing. The area is characterized by strong climatic gradients, with high rates of precipitation on the southwestern side of the range and dry conditions on the northern side. Glaciers on the northern and

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25

Allmendinger, Richard W., and Gabriel González. "Invited review paper: Neogene to Quaternary tectonics of the coastal Cordillera, northern Chile." Tectonophysics 495, no. 1-2 (2010): 93–110. http://dx.doi.org/10.1016/j.tecto.2009.04.019.

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26

Holmlund, Per, and Humberto Fuenzalida. "Anomalous glacier responses to 20th century climatic changes in Darwin Cordillera, southern Chile." Journal of Glaciology 41, no. 139 (1995): 465–73. http://dx.doi.org/10.3189/s0022143000034808.

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AbstractThere is an asymmetric pattern response of glaciers in Darwin Cordillera (54–55° S, 69–71° W) to the climate of the 20th century. This asymmetry is suggested here as a cause of an increased wind activity which has a pronounced orographic effect. Although climatic records for the last 50 years show a warming trend, as well as no trend in precipitation in the area, some glaciers are advancing. The area is characterized by strong climatic gradients, with high rates of precipitation on the southwestern side of the range and dry conditions on the northern side. Glaciers on the northern and

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27

Izagirre, Eñaut, Christopher M. Darvill, Camilo Rada, and Juan Carlos Aravena. "Glacial geomorphology of the Marinelli and Pigafetta glaciers, Cordillera Darwin Icefield, southernmost Chile." Journal of Maps 14, no. 2 (2018): 269–81. http://dx.doi.org/10.1080/17445647.2018.1462264.

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28

Solervicens, Jaime. "Descripción de un nuevo género y especie de Salpinginae (Coleoptera: Salpingidae) para Chile." REVISTA CHILENA DE ENTOMOLOGÍA 47, no. 1 (2021): 9–18. http://dx.doi.org/10.35249/rche.47.1.21.02.

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Basado en material recolectado en la cordillera de Nahuelbuta (provincias de Malleco y Arauco) se describe un nuevo género y especie de Salpingidae de Chile. Se presentan imágenes del adulto de la especie y de detalles de la cabeza y el tórax, además de figuras de las piezas bucales, alas y órganos genitales del macho y de la hembra. Se destacan sus caracteres diagnósticos y se establecen diferencias y afinidad con otros géneros de la familia.

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29

Gutiérrez Caro, Braulio. "Influencia del origen de las semillas en el desempeño de coigüe (Nothofagus dombeyi (Mirb.) Oerst.) en ensayos de 15 años en la costa y precordillera de la Región de Los Ríos." Ciencia & Investigación Forestal 26, no. 2 (2020): 31–44. http://dx.doi.org/10.52904/0718-4646.2020.531.

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Se caracteriza el desempeño de coigüe, en términos de supervivencia, altura, diámetro y rectitud de fuste a los 14-15 años de edad en dos ensayos establecidos en costa y pre cordillera de la región de Los Ríos Chile (Huillilemu en San José de la Mariquina y Remeco en Panguipulli); se analiza también el efecto del origen de las semillas (zonas de procedencias) sobre las variables mencionadas.

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30

Melkonian, A. K., M. J. Willis, M. E. Pritchard, A. Rivera, F. Bown, and S. A. Bernstein. "Satellite-derived volume loss rates and glacier speeds for the Cordillera Darwin Icefield, Chile." Cryosphere 7, no. 3 (2013): 823–39. http://dx.doi.org/10.5194/tc-7-823-2013.

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Abstract. We produce the first icefield-wide volume change rate and glacier velocity estimates for the Cordillera Darwin Icefield (CDI), a 2605 km2 temperate icefield in southern Chile (69.6° W, 54.6° S). Velocities are measured from optical and radar imagery between 2001–2011. Thirty-six digital elevation models (DEMs) from ASTER and the SRTM DEM are stacked and a weighted linear regression is applied to elevations on a pixel-by-pixel basis to estimate volume change rates. The CDI lost mass at an average rate of −3.9 ± 1.5 Gt yr−1 between 2000 and 2011, equivalent to a sea level rise (SLR) of

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31

Melkonian, A. K., M. J. Willis, M. E. Pritchard, A. Rivera, F. Bown, and S. A. Bernstein. "Satellite-Derived Volume Loss Rates and Glacier Speeds for the Cordillera Darwin Icefield, Chile." Cryosphere Discussions 6, no. 4 (2012): 3503–38. http://dx.doi.org/10.5194/tcd-6-3503-2012.

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Abstract. We produce the first icefield-wide volume change rate and glacier velocity estimates for the Cordillera Darwin Icefield (CDI), a 2605 km2 temperate icefield in Southern Chile (69.6° W, 54.6° S). Velocities are measured from optical and radar imagery between 2001–2011. Thirty-seven digital elevation models (DEMs) from ASTER and the SRTM are stacked and a weighted linear regression is applied to elevations on a pixel-by-pixel basis to estimate volume change rates. The CDI lost mass at an average rate of 3.9 ± 0.3 Gt yr−1 between 2000 and 2011, equivalent to a sea level rise (SLR) of 0.

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32

Soto-Rogel, Pamela, and Juan Carlos Aravena. "Potencial dendroclimático de Nothofagus betuloides en la Cordillera de Darwin, Tierra del Fuego, Chile." Bosque (Valdivia) 38, no. 1 (2017): 155–68. http://dx.doi.org/10.4067/s0717-92002017000100016.

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33

Alvarez, P. Pamela, and Victor A. Ramos. "The Mercedario rift system in the principal Cordillera of Argentina and Chile (32° SL)." Journal of South American Earth Sciences 12, no. 1 (1999): 17–31. http://dx.doi.org/10.1016/s0895-9811(99)00004-8.

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34

Cornejo B., Luis E., and Lorena Sanhueza R. "Coexistencia de Cazadores Recolectores y Horticultores Tempranos en la Cordillera Andina de Chile Central." Latin American Antiquity 14, no. 4 (2003): 389–407. http://dx.doi.org/10.2307/3557575.

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Recientes estudios en la cordillera andina de Chile Central nos han permitido identificar la coexistencia de dos modos de vida distintos en el mismo territorio durante el período Alfarero Temprano (350 a.C. a 900 d.C). Estos dos modos de vida corresponden, por un lado, a poblaciones de cazadores recolectores continuadores de la tradición Arcaica, especialmente en los aspectos económicos y en la tecnología lítica orientada curatorialmente, pero poseedores de algunas vasijas de cerámica adquiridas desde otros grupos propiamente alfareros y, por otro lado, a poblaciones semi-sedentarias con una e

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35

Irwin, James J., Warren D. Sharp, Robert R. Spangler, and Robert E. Drake. "Some paleomagnetic constraints on the tectonic evolution of the coastal cordillera of central Chile." Journal of Geophysical Research 92, B5 (1987): 3603. http://dx.doi.org/10.1029/jb092ib05p03603.

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36

Mernild, Sebastian H., Glen E. Liston, Christopher A. Hiemstra, Jacob C. Yde, James McPhee, and Jeppe K. Malmros. "The Andes Cordillera. Part II: Rio Olivares Basin snow conditions (1979-2014), central Chile." International Journal of Climatology 37, no. 4 (2016): 1699–715. http://dx.doi.org/10.1002/joc.4828.

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37

Hartley, A. J., P. Turner, G. D. Williams, and S. Flint. "Palaeomagnetism of the Cordillera de la Costa, northern Chile: evidence for local forearc rotation." Earth and Planetary Science Letters 89, no. 3-4 (1988): 375–86. http://dx.doi.org/10.1016/0012-821x(88)90124-0.

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38

Alloatti, Norma. "Mis impresiones y mis vicisitudes en mi viaje a Europa pasando por el Estrecho de Magallanes y en mi excursión a Buenos Aires pasando por la cordillera de Los Andes." La Manzana de la Discordia 9, no. 2 (2016): 115. http://dx.doi.org/10.25100/lamanzanadeladiscordia.v9i2.1609.

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De la Barra, Maipina (2013)Mis impresiones y mis vicisitudes en mi viaje a Europa pasando por el Estrecho de Magallanes y en mi excursión a Buenos Aires pasando por la cordillera de Los AndesReedición crítica del original publicado en 1878 a cargo de Carla Ulloa Inostroza (Transcripción, actualización ortográfica y estudio preliminar).Santiago, Chile, Editorial Cuarto Propio, diciembre 2013, 224 páginas,ISBN. 978-956-260-663-9.

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39

Encinas, Alfonso, Victor Maksaev, Luisa Pinto, Jacobus P. Le Roux, Francisco Munizaga, and Marcos Zentilli. "Pliocene lahar deposits in the Coastal Cordillera of central Chile: Implications for uplift, avalanche deposits, and porphyry copper systems in the Main Andean Cordillera." Journal of South American Earth Sciences 20, no. 4 (2006): 369–81. http://dx.doi.org/10.1016/j.jsames.2005.08.007.

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40

Sarricolea, Pablo, Mariajosé Herrera Ossandon, and Cristóbal Araya Escobar. "Análisis de la concentración diaria de las precipitaciones en Chile central y su relación con la componente zonal (subtropicalidad) y meridiana (orográfica)." Investigaciones Geográficas, no. 45 (August 21, 2013): 37. http://dx.doi.org/10.5354/0719-5370.2013.27595.

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Este artículo analiza la distribución espacial y temporal de la irregularidad de las precipitaciones diarias en una franja zonal de la región central de Chile (32°50’S-34°12’S), mediante el índice de concentración (CI). En total se calculó el CI para un total de 16 estaciones meteorológicas, en el período 1965-2010. El propósito fue generar una regionalización climática basada en un índice diario que mide la irregularidad de las precipitaciones. Teóricamente, se han ensayado dos hipótesis:la primera propone que el CI disminuye de Norte-Sur, asociado a la componente Subtropicalidad; la segunda

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41

A. Drake, Lawrence, and Estela Minaya Ramos. "The propagation of Love and Rayleigh waves in the Andean Region." Geofísica Internacional 35, no. 3 (1996): 273–84. http://dx.doi.org/10.22201/igeof.00167169p.1996.35.3.462.

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El patrón distintivo desde la fuente sísmica de un campo irradiado de ondas sísmicas se modifica profundamente al pasar por una región irregular como la Cordillera de los Andes de América del Sur. La onda Lg guiada por la corteza útil en la discriminación de fuentes sísmicas, pero, aun para una sola fuente, las amplitudes de ondas de periódo corto como Lg pueden variar significativamente. La Cordillera de los Andes de Bolivia forma una parte de la cadea de los Andes, que se originó en los dos principales ciclos orogénicos del Fanerozoico, un Ciclo Preandino Precámbrico-Paleozoico Superior y el

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Koch, Johannes. "Little Ice Age and recent glacier advances in the Cordillera Darwin, Tierra del Fuego, Chile." Anales del Instituto de la Patagonia 43, no. 1 (2015): 127–36. http://dx.doi.org/10.4067/s0718-686x2015000100011.

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Urra, Francisco. "Tenoia floresi, una nueva especie de Autostichidae (Lepidoptera: Gelechioidea) de la cordillera de Nahuelbuta, Chile." REVISTA CHILENA DE ENTOMOLOGÍA 46, no. 2 (2020): 205–9. http://dx.doi.org/10.35249/rche.46.2.20.11.

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Herrera, Christian, Carolina Gamboa, Emilio Custodio, et al. "Groundwater origin and recharge in the hyperarid Cordillera de la Costa, Atacama Desert, northern Chile." Science of The Total Environment 624 (May 2018): 114–32. http://dx.doi.org/10.1016/j.scitotenv.2017.12.134.

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González, Gabriel, José Cembrano, Daniel Carrizo, Alejandro Macci, and Heinz Schneider. "The link between forearc tectonics and Pliocene–Quaternary deformation of the Coastal Cordillera, northern Chile." Journal of South American Earth Sciences 16, no. 5 (2003): 321–42. http://dx.doi.org/10.1016/s0895-9811(03)00100-7.

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Halama, Ralf, and Matthias Konrad-Schmolke. "Retrograde metasomatic effects on phase assemblages in an interlayered blueschist–greenschist sequence (Coastal Cordillera, Chile)." Lithos 216-217 (February 2015): 31–47. http://dx.doi.org/10.1016/j.lithos.2014.12.004.

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KOHN, M. J., F. S. SPEAR, and I. W. D. DALZIEL. "Metamorphic P-T Paths from Cordillera Darwin, a Core Complex in Tierra del Fuego, Chile." Journal of Petrology 34, no. 3 (1993): 519–42. http://dx.doi.org/10.1093/petrology/34.3.519.

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Vanneste, Heleen, François De Vleeschouwer, Sébastien Bertrand, et al. "Elevated dust deposition in Tierra del Fuego (Chile) resulting from Neoglacial Darwin Cordillera glacier fluctuations." Journal of Quaternary Science 31, no. 7 (2016): 713–22. http://dx.doi.org/10.1002/jqs.2896.

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Frutos J, Jose, and Guillermo Alfaro H. "Metallogenic and tectonic characteristics of the paleozoic ophiolitic belt of the southern Chile coastal Cordillera." Geologische Rundschau 76, no. 2 (1987): 343–56. http://dx.doi.org/10.1007/bf01821079.

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González, Mauro E., and Thomas T. Veblen. "Climatic influences on fire inAraucaria araucana–Nothofagusforests in the Andean cordillera of south-central Chile." Écoscience 13, no. 3 (2006): 342–50. http://dx.doi.org/10.2980/i1195-6860-13-3-342.1.

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