With a Focus on Lascar Volcano
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Appendix A. Supplementary Material to the Manuscript
Appendix A. Supplementary material to the manuscript: The role of crustal and eruptive processes versus source variations in controlling the oxidation state of iron in Central Andean magmas 1. Continental crust beneath the CVZ Country Rock The basement beneath the sampled portion of the CVZ belongs to the Paleozoic Arequipa- Antofalla terrain – a high temperature metamorphic terrain with abundant granitoid intrusions that formed in response to Paleozoic subduction (Lucassen et al., 2000; Ramos et al., 1986). In Northern Chile and Northwestern Argentina this Paleozoic metamorphic-magmatic basement is largely homogeneous and felsic in composition, consistent with the thick, weak, and felsic properties of the crust beneath the CVZ (Beck et al., 1996; Fig. A.1). Neodymium model ages of exposed Paleozoic metamorphic-magmatic basement and sediments suggest a uniform Proterozoic protolith, itself derived from intrusions and sedimentary rock (Lucassen et al., 2001). AFC Model Parameters Pervasive assimilation of continental crust in the Central Andean ignimbrite magmas is well established (Hildreth and Moorbath, 1988; Klerkx et al., 1977; Fig. A.1) and has been verified by detailed analysis of radiogenic isotopes (e.g. 87Sr/86Sr and 143Nd/144Nd) on specific systems within the CVZ (Kay et al., 2011; Lindsay et al., 2001; Schmitt et al., 2001; Soler et al., 2007). Isotopic results indicate that the CVZ magmas are the result of mixing between a crustal endmember, mainly gneisses and plutonics that have a characteristic crustal signature of high 87Sr/86Sr and low 145Nd/144Nd, and the asthenospheric mantle (low 87Sr/86Sr and high 145Nd/144Nd; Fig. 2). In Figure 2, we model the amount of crustal assimilation required to produce the CVZ magmas that are targeted in this study. -
El Volcán Chiliques Y El" Morar-En-El-Mundo" De Una
Estudios Atacameños ISSN: 0716-0925 [email protected] Universidad Católica del Norte Chile Moyano, Ricardo; Uríbe, Carlos El volcán chiliques y el "morar-en-el-mundo" de una comunidad atacameña del norte de Chile Estudios Atacameños, núm. 43, 2012, pp. 187-208 Universidad Católica del Norte San Pedro de Atacama, Chile Disponible en: http://www.redalyc.org/articulo.oa?id=31526842010 Cómo citar el artículo Número completo Sistema de Información Científica Más información del artículo Red de Revistas Científicas de América Latina, el Caribe, España y Portugal Página de la revista en redalyc.org Proyecto académico sin fines de lucro, desarrollado bajo la iniciativa de acceso abierto EL VOLCÁN CHILIQUES y EL "MORAR-EN-EL MUNDO" DE UNA COMUNIDAD ATACAMEÑA DEL NORTE DE CHILE Ricardo Moyana' y Carlos Uríbe' --+ INTRODUCCIÓN Resumen El volcán Chiliques corresponde a un estrato volcán de En estetrabajosemuestranlosresul tadospreliminares del 5778 rn.s.n.rn., ubicado en la Región de Antofagasta. reconocimiento arqueológico delvolcán Chílíques (2}034'5 /67°42'W /5778 m.s.nm.), desierto deAtacama, nortedeChile. El objetivo fue norte de Chile (23'34'5, 6i42'W) (Figura 1). Esta mon confirmar laexistencia desitiosarqueológicos enlazona, asícomo taña no habría registrado actividad volcánica durante los una posible líneaceque proyectadadesdeelcentroceremonial de últimos 10.000 años, sin embargo, en enero de 2002 Socaire. Los resul tadosconfirman laimportancia delvolcán Chiliques una imagen infrarroja obtenida por ASTER (Advanced como propiciadordefenómenos meteorológicos dentrodelsistema de Spaceborne Thermal Emission and Reflection Radio montañassagradas invocadas para laceremoníade limpia decanalesdel mesdeoctubreenSocaire. Chílíques habríaconstituidoun "axis mund¡' meter) de la NASA, reveló ciertos hotspots en una zona porlassiguientes razones: su forma cónica yvisibilidad permanente cercana al cráter y edificiovolcánico.' desdeotrosadoratorios prehíspánícos. -
Iv BOLIVIA the Top of the World
iv BOLIVIA The top of the world Bolivia takes the breath away - with its beauty, its geographic and cultural diversity, and its lack of oxygen. From the air, the city of La Paz is first glimpsed between two snowy Andean mountain ranges on either side of a plain; the spread of the joined-up cities of El Alto and La Paz, cradled in a huge canyon, is an unforgettable sight. For passengers landing at the airport, the thinness of the air induces a mixture of dizziness and euphoria. The city's altitude affects newcomers in strange ways, from a mild headache to an inability to get up from bed; everybody, however, finds walking up stairs a serious challenge. The city's airport, in the heart of El Alto (literally 'the high place'), stands at 4000 metres, not far off the height of the highest peak in Europe, Mont Blanc. The peaks towering in the distance are mostly higher than 5000m, and some exceed 6000m in their eternally white glory. Slicing north-south across Bolivia is a series of climatic zones which range from tropical lowlands to tundra and eternal snows. These ecological niches were exploited for thousands of years, until the Spanish invasion in the early sixteenth century, by indigenous communities whose social structure still prevails in a few ethnic groups today: a single community, linked by marriage and customs, might live in two or more separate climes, often several days' journey away from each other on foot, one in the arid high plateau, the other in a temperate valley. -
Volcán Lascar
Volcán Lascar Región: Antofagasta Provincia: El Loa Comuna: San Pedro de Atacama Coordenadas: 21°22’S – 67°44’O Poblados más cercanos: Talabre – Camar – Socaire Tipo: Estratovolcán Altura: 5.592 m s.n.m. Diámetro basal: 8.9 km Área basal: 62.2 km2 Volumen estimado: 28.5 km3 Última actividad: 2015 Última erupción mayor: 1993 Volcán Lascar. Vista desde el norte Ranking de riesgo (Fotografía: Gabriela Jara, SERNAGEOMIN) 14 específico: Generalidades El volcán Láscar corresponde a un estratovolcán compuesto, elongado en dirección este-oeste, activo desde hace unos 240 ka y emplazado en el margen oeste de la planicie altiplánica. Está conformado por lavas andesíticas, que alcanzan más de 10 km de longitud, y por potentes lavas dacíticas que se extienden hasta 5 km, las que fueron emitidas desde los flancos NO a SO. La lava más reciente se estima en 7 mil años de antigüedad. En los alrededores del volcán se reconocen depósitos de flujo y caída piroclástica, además de numerosos cráteres de impacto asociados a la eyección de bombas durante erupciones plinianas y subplinianas. El principal evento eruptivo durante su evolución se denomina Ignimbrita Soncor, generado hace unos 27 ka al oeste del volcán y con un volumen estimado cercano a los 10 km3. En la cima de este volcán se observan seis cráteres, algunos anidados, y el central de estos se encuentra activo. Registro eruptivo Este volcán ha presentado alrededor de 30 erupciones explosivas desde el siglo XIX, lo que lo convierte en el volcán más activo del norte de Chile. Estos eventos han consistido típicamente en erupciones vulcanianas de corta duración, con emisión de ceniza fina y proyecciones balísticas en un radio de 5 km, donde el último evento de este tipo ocurrió el 30 de octubre del 2015. -
Vegetation and Climate Change on the Bolivian Altiplano Between 108,000 and 18,000 Years Ago
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by DigitalCommons@University of Nebraska University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Earth and Atmospheric Sciences, Department Papers in the Earth and Atmospheric Sciences of 1-1-2005 Vegetation and climate change on the Bolivian Altiplano between 108,000 and 18,000 years ago Alex Chepstow-Lusty Florida Institute of Technology, [email protected] Mark B. Bush Florida Institute of Technology Michael R. Frogley Florida Institute of Technology, 150 West University Boulevard, Melbourne, FL Paul A. Baker Duke University, [email protected] Sherilyn C. Fritz University of Nebraska-Lincoln, [email protected] See next page for additional authors Follow this and additional works at: https://digitalcommons.unl.edu/geosciencefacpub Part of the Earth Sciences Commons Chepstow-Lusty, Alex; Bush, Mark B.; Frogley, Michael R.; Baker, Paul A.; Fritz, Sherilyn C.; and Aronson, James, "Vegetation and climate change on the Bolivian Altiplano between 108,000 and 18,000 years ago" (2005). Papers in the Earth and Atmospheric Sciences. 30. https://digitalcommons.unl.edu/geosciencefacpub/30 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Papers in the Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Authors Alex Chepstow-Lusty, Mark B. Bush, Michael R. Frogley, Paul A. Baker, Sherilyn C. Fritz, and James Aronson This article is available at DigitalCommons@University of Nebraska - Lincoln: https://digitalcommons.unl.edu/ geosciencefacpub/30 Published in Quaternary Research 63:1 (January 2005), pp. -
Seasonal Patterns of Atmospheric Mercury in Tropical South America As Inferred by a Continuous Total Gaseous Mercury Record at Chacaltaya Station (5240 M) in Bolivia
Atmos. Chem. Phys., 21, 3447–3472, 2021 https://doi.org/10.5194/acp-21-3447-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Seasonal patterns of atmospheric mercury in tropical South America as inferred by a continuous total gaseous mercury record at Chacaltaya station (5240 m) in Bolivia Alkuin Maximilian Koenig1, Olivier Magand1, Paolo Laj1, Marcos Andrade2,7, Isabel Moreno2, Fernando Velarde2, Grover Salvatierra2, René Gutierrez2, Luis Blacutt2, Diego Aliaga3, Thomas Reichler4, Karine Sellegri5, Olivier Laurent6, Michel Ramonet6, and Aurélien Dommergue1 1Institut des Géosciences de l’Environnement, Université Grenoble Alpes, CNRS, IRD, Grenoble INP, Grenoble, France 2Laboratorio de Física de la Atmósfera, Instituto de Investigaciones Físicas, Universidad Mayor de San Andrés, La Paz, Bolivia 3Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, 00014, Finland 4Department of Atmospheric Sciences, University of Utah, Salt Lake City, UT 84112, USA 5Université Clermont Auvergne, CNRS, Laboratoire de Météorologie Physique, UMR 6016, Clermont-Ferrand, France 6Laboratoire des Sciences du Climat et de l’Environnement, LSCE-IPSL (CEA-CNRS-UVSQ), Université Paris-Saclay, Gif-sur-Yvette, France 7Department of Atmospheric and Oceanic Sciences, University of Maryland, College Park, MD 20742, USA Correspondence: Alkuin Maximilian Koenig ([email protected]) Received: 22 September 2020 – Discussion started: 28 October 2020 Revised: 20 January 2021 – Accepted: 21 January 2021 – Published: 5 March 2021 Abstract. High-quality atmospheric mercury (Hg) data are concentrations were linked to either westerly Altiplanic air rare for South America, especially for its tropical region. As a masses or those originating from the lowlands to the south- consequence, mercury dynamics are still highly uncertain in east of CHC. -
Scale Deformation of Volcanic Centres in the Central Andes
letters to nature 14. Shannon, R. D. Revised effective ionic radii and systematic studies of interatomic distances in halides of 1–1.5 cm yr21 (Fig. 2). An area in southern Peru about 2.5 km and chalcogenides. Acta Crystallogr. A 32, 751–767 (1976). east of the volcano Hualca Hualca and 7 km north of the active 15. Hansen, M. (ed.) Constitution of Binary Alloys (McGraw-Hill, New York, 1958). 21 16. Emsley, J. (ed.) The Elements (Clarendon, Oxford, 1994). volcano Sabancaya is inflating with U LOS of about 2 cm yr . A third 21 17. Tanaka, H., Takahashi, I., Kimura, M. & Sobukawa, H. in Science and Technology in Catalysts 1994 (eds inflationary source (with ULOS ¼ 1cmyr ) is not associated with Izumi, Y., Arai, H. & Iwamoto, M.) 457–460 (Kodansya-Elsevier, Tokyo, 1994). a volcanic edifice. This third source is located 11.5 km south of 18. Tanaka, H., Tan, I., Uenishi, M., Kimura, M. & Dohmae, K. in Topics in Catalysts (eds Kruse, N., Frennet, A. & Bastin, J.-M.) Vols 16/17, 63–70 (Kluwer Academic, New York, 2001). Lastarria and 6.8 km north of Cordon del Azufre on the border between Chile and Argentina, and is hereafter called ‘Lazufre’. Supplementary Information accompanies the paper on Nature’s website Robledo caldera, in northwest Argentina, is subsiding with U (http://www.nature.com/nature). LOS of 2–2.5 cm yr21. Because the inferred sources are more than a few kilometres deep, any complexities in the source region are damped Acknowledgements such that the observed surface deformation pattern is smooth. -
Lake-Level Chronology on the Southern Bolivian Altiplano
Quaternary Research 51,54-66 (1999) D Article ID qres.1998.2017, available online at http://www.idealibrary.com on I bk@ E 9. Lake-Level Chronology on the Southern Bolivian Altiplano (1 8"-23"s) during Late-Glacial Time and the Early Holocene Florence Sylvestre Université d'Angers, Laboratoire de Géologie, 2, boulevard Lavoisier, 49045 Angers Cedex, France Michel Servant ORSTOM, 32, avenue Henri Varagnat, 93143 Bondy Cedex, France Simone Servant-Vildary ORSTOM-MNHN, Laboratoire de Géologie, 43, rue Buffon, 75005 Paris Cedex, France Christiane Causse . LSCE (UMR CNRS-CEA), avenue de la Terrasse, 91198 Gif-sur-Yvette Cedex, France Marc Fournier IPSNI-WMRE, Bat. 501, Bois des Rames, 91400 Orsay Cedex, France and - - __ .- . <- ~ .__ i -- II Jean-Pierre Ybert 11 STON, 32, avenue Henri Varagnat 93143 Bondy Cedex, France 002 1851 O1 Received December 11, 1997 .-.lul~lo~~~1SliEl;unll I : I powerful tool for paleoclimatic reconstructions if a good chro- - Stratigraphic analyses of outcrops, shorelines,I and diatoms from nology can be obtained. Significant changes in lake levels the southern Bolivian Altiplano (Uyuni-Coipasa basin) reveal two occurred on the southern Bolivian Altiplano (Uyuni-Coipasa major lacustrine phases during the late-glacial period and the basin) during the late-glac.al period. A large lake (L,~T~~~~) early Holocene, based on a chronology established by radiocarbon filled the closed basin where salars (salt pans) now exist and U/Th control. A comparison of I4C and zs0Th/234Uages shows that during times of high lake level, radiocarbon ages are valid. (Servant and Fontes, 1978). The timing of lake-level changes However, during low-water periods, I4Cages must be corrected for has been based on rxh~arbo~dating Of gastropod a reservoir effect. -
Argentine National Report 1999-2003
REPÚBLICA ARGENTINA INFORME NACIONAL PRESENTADO A LA ASOCIACIÓN INTERNACIONAL DE VOLCANOLOGÍA Y QUÍMICA DEL INTERIOR DE LA TIERRA –IAVCEI– XXIV. ASAMBLEA GENERAL DE LA UNIÓN GEODÉSICA Y GEOFÍSICA INTERNACIONAL – UGGI – Perugia, Italia, 2 – 13 julio de 2007 -------------------- --------------------- ARGENTINA REPUBLIC NATIONAL REPORT PRESENTED TO THE INTERNATONAL ASSOCIATION OF VOLCANOLOGY AND CHEMISTRY OF THE EARTH INTERIOR –IAVCEI– XXIV GENERAL ASSEMBLY OF THE INTERNATIONAL UNION OF GEODESY AND GEOPHYSICS – IUGG – Perugia, Italy, 2 – 13 July, 2007 --------------------------------------------------------------------------------------------- COMITÉ NACIONAL DE LA UNIÓN GEODÉSICA Y GEOFÍSICA INTERNACIONAL NATIONAL COMMITTEE OF THE INTERNATIONAL UNION OF GEODESY AND GEOPHYSICS ------------------------------------------------------------------- ARGENTINA 2007 REPÚBLICA ARGENTINA COMITÉ NACIONAL DE LA UNIÓN GEODÉSICA Y GEOFÍSICA INTERNACIONAL (CNUGGI) ARGENTINA REPUBLIC NATIONAL COMMITTEE OF THE INTERNATIONAL UNION OF GEODESY AND GEOPHYSICS The main function of the IUGG National Committee is representing the Union in Argentina. It is chaired by the Military Geographic Institute Director, and assisted by two Vice Presidents, a General Secretary and a Secretary Assistant. The current (2007) head staff is as follows: President: Cnl. VGM Eng. Alfredo Augusto Stahlschmidt Executive 1st Vicepresident: Dr Corina Risso 2nd Vicepresident: Dr Nora Sabbione General Secretary: Surv. Rubén Carlos Ramos Secretary Assistant: Surv. Sergio Rubén Cimbaro Treasurer: -
Chiodi Et Al 2019.Pdf
Journal of South American Earth Sciences 94 (2019) 102213 Contents lists available at ScienceDirect Journal of South American Earth Sciences journal homepage: www.elsevier.com/locate/jsames Preliminary conceptual model of the Cerro Blanco caldera-hosted geothermal system (Southern Puna, Argentina): Inferences from T geochemical investigations ∗ A. Chiodia, , F. Tassib,c, W. Báeza, R. Filipovicha, E. Bustosa, M. Glok Gallid, N. Suzañoe, Ma. F. Ahumadaa, J.G. Viramontea, G. Giordanof,g, G. Pecorainoh, O. Vasellib,c a Instituto de Bio y Geociencias del NOA (IBIGEO, UNSa-CONICET), Av. 9 de Julio14, A4405BBA Salta, Argentina b Department of Earth Sciences, University of Florence, Via La Pira 4, 50121 Florence, Italy c CNR-IGG Institute of Geosciences and Earth Resources, Via La Pira 4, 50121 Florence, Italy d Centro de Investigaciones en Física e Ingeniería del Centro de la Provincia de Buenos Aires (CIFICEN), Pinto 399, 7000, Buenos Aires, Argentina e Universidad Nacional de Jujuy, Argentina f Department of Sciences, University Roma Tre, 00146 Rome, Italy g CNR-IDPA Institute for Dynamics of Environmental Processes, Via M. Bianco, 20131 Milan, Italy h Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione di Palermo, Via Ugo La Malfa 153, 90146, Palermo, Italy ARTICLE INFO ABSTRACT Keywords: The Cerro Blanco Caldera (CBC) is the youngest collapse caldera system in the Southern Central Andes (Southern Hydrothermal system Puna, Argentina). The CBC is subsiding with at an average velocity of 0.87 cm/year and hosts an active geo- Fluid geochemistry thermal system. A geochemical characterization of emitted fluids was carried out based on the chemical and Geothermal prospection isotopic compositions of fumaroles, and thermal and cold springs discharged in this volcanic area with the aim of Quaternary caldera constructing the first hydrogeochemical conceptual model and preliminary estimate the geothermal potential. -
Processes Culminating in the 2015 Phreatic Explosion at Lascar Volcano, Chile, Monitored by Multiparametric Data Ayleen Gaete1, Thomas R
https://doi.org/10.5194/nhess-2019-189 Preprint. Discussion started: 25 June 2019 c Author(s) 2019. CC BY 4.0 License. Processes culminating in the 2015 phreatic explosion at Lascar volcano, Chile, monitored by multiparametric data Ayleen Gaete1, Thomas R. Walter1, Stefan Bredemeyer1,2, Martin Zimmer1, Christian Kujawa1, Luis Franco3, Juan San Martin4, Claudia Bucarey Parra3 5 1 GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany 2 GEOMAR Helmholtz Centre for Ocean Research Kiel, 24148 Kiel, Germany 3 Observatorio Volcanológico de Los Andes del Sur (OVDAS), Servicio Nacional de Geología y Minería (SERNAGEOMIN), Temuco, Chile. 4 Physics Science Department, Universidad de la Frontera, Casilla 54-D, Temuco, Chile. 10 Correspondence to: Ayleen Gaete ([email protected]) Abstract. Small steam-driven volcanic explosions are common at volcanoes worldwide but are rarely documented or monitored; therefore, these events still put residents and tourists at risk every year. Steam-driven explosions also occur frequently (once every 2-5 years on average) at Lascar volcano, Chile, where they are often spontaneous and lack any identifiable precursor activity. Here, for the first time at Lascar, we describe the processes culminating in such a sudden 15 volcanic explosion that occurred on October 30, 2015, which was thoroughly monitored by cameras, a seismic network, and gas (SO2 and CO2) and temperature sensors. Prior to the eruption, we retrospectively identified unrest manifesting as a gradual increase in the number of long-period (LP) seismic events in 2014, indicating an augmented level of activity at the volcano. Additionally, SO2 flux and thermal anomalies were detected before the eruption. -
00-P. P.Ginas + Editorial
Estudios Atacameños Nº 16 - 1998 La tradición surandina del desierto: Etnobotánica del área del Salar de Atacama (Provincia de El Loa, Región de Antofagasta, Chile)1 CAROLINA VILLAGRÁN*, VICTORIA CASTRO**, GILBERTO SÁNCHEZ***, MARCELA ROMO**, CLAUDIO LATORRE** y LUIS FELIPE HINOJOSA** RESUMEN El área del Salar de Atacama, Provincia de El Loa, to de las plantas en los territorios de estas culturas segunda Región de Antofagasta del norte de Chi- y definir sus singularidades etnobotánicas, en co- le, es una de las más secas del mundo, correspon- rrespondencia con su situación tan especial den- diendo al área de máxima penetración del Desier- tro de los Andes del norte de Chile. Con este pro- to de Atacama en la costa Pacífica de Sudamérica. pósito, se realizó una recolección exhaustiva de la En efecto, y en concordancia con la disminución flora del área y un muestreo sistemático de la ve- de las lluvias en sentido NW-SE, desde los Andes getación, este último siguiendo un transecto de Arica (18°S), hacia los de Antofagasta (24°S), altitudinal desde el Salar de Atacama (2.700 m) se observa que la vegetación se retrae paulatina- hasta el Salar de Aguas Calientes (4.500 m). Pos- mente hacia mayores altitudes. Así, extensas áreas teriormente, se entrevistaron 38 personas prove- al interior de la ciudad de Calama, representadas nientes de San Pedro de Atacama, Toconao, por el Salar de Atacama, Cordillera de Domeyko Talabre, Camar, Socaire y Peine. y sectores bajos de la vertiente occidental andina corresponden a desiertos ‘absolutos’, con valores Para las 173 especies de plantas consultadas se de coberturas de plantas vasculares prácticamen- registraron 416 nombres vernaculares, correspon- te nulos.