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El Paso De Los Andes, Camino a Través De Cuatro Cordilleras. Conferencia
;V'-- ' ■ ' ’S ■>^; 'SíA-v . MUSEO HISTÓRICO NACIONAL , rí^r..,-- Núm. XII EL PASO DE LOS ANDES, CAMIÑO A TRAVES DE CUATRO CORDILLERAS CONFERENCIA PRONUNCIADA EL 17 DE AGOSTO DE 1948 PO K EL Dr. EDUARDO ACEVEDO DÍAZ /I’ PRECEDIDA POR EL DISCURSO DEL DIRECTOR DEL MUSEO £ HISTÓRICO NACIONAL, PROFESOR DON ANTONIO APRAIZ u^ A ■Ñ 1?^?l ■ 1 9 4 8 TALLERES GRAFICOS “ VIGOR’^ BUENOS AIRES ÜEX BICC T S-6019 Biblioteca de la Universidad de Extremadura Biblioteca de la Universidad de Extremadura , ¿ r ür ^^10 EL PASO DE I-OS ANDES, CAMINO A TRAVÉS DE CUATRO CORDILLERAS a: I r A A jNIVERSIDflD .n£. EXTREnflBUafl. Biblioteca de la Universidad de Extremadura 7l'ZD2000"563972' D IS rRIF.UC10x\ GRATUITA TaUeres Gráficos “ Vigor", Ahina j 7j , Buenos Aires. Diciembre )0 de I9Í9. Biblioteca de la Universidad de Extremadura Presidente de la Nación G eneral J uan P erón Secretario de Educación l’ ROFESOR D octor O scar I vanissevich Subsecretario de Cultura Sr. A ntonio P. C astro COMISION NACIONAL de MUSEOS y de MONUMENTOS Y LUGARES HISTORICOS Presidente D r . Eduardo A cevf.do D íaz Vocales Señor Director del Museo Histórico Nacional P rofesor D on A ntonio A praiz Señor Director Interino del Museo Histórico Sarmiento D on G u illerm o A im o Señor Director del Museo Mitre D on J uan A ngel F arini Teniente C oronel José Ignacio Iturralde Señor Interventor de la Dirección Nacional de Arquitectura G eneral de D ivisión R odolfo M artínez P ita Señor Director de la Biblioteca Nacional D r . -
Lpzsttz Et Al Final Ms.Pdf
Lithium and Brine Geochemistry in the Salars of the Southern Puna, Andean Plateau of Argentina Romina Lucrecia Lopez Steinmetz, Stefano Salvi, Carisa Sarchi, Carla Santamans, Lorena Cecilia Lopez Steinmetz To cite this version: Romina Lucrecia Lopez Steinmetz, Stefano Salvi, Carisa Sarchi, Carla Santamans, Lorena Cecilia Lopez Steinmetz. Lithium and Brine Geochemistry in the Salars of the Southern Puna, Andean Plateau of Argentina. Economic Geology, Society of Economic Geologists, 2020, 115, pp.1079 - 1096. 10.5382/econgeo.4754. hal-02989895 HAL Id: hal-02989895 https://hal.archives-ouvertes.fr/hal-02989895 Submitted on 5 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 Lithium and Brine Geochemistry in the Salars of the Southern Puna, 2 Andean Plateau of Argentina 3 4 Romina Lucrecia López Steinmetz 1 *, Stefano Salvi 2 , Carisa Sarchi 1 , Carla Santamans 1 , 5 Lorena Cecilia López Steinmetz 3 6 7 1 CONICET (INECOA), Instituto de Geología y Minería, Universidad Nacional de Jujuy, Av. 8 Bolivia 1661, S.S. de Jujuy 4600, Argentina 9 2 Université de Toulouse, CNRS, GET, IRD, OMP, 14 Av. Edouard Belin, Toulouse 31400, 10 France 11 3 Instituto de Investigaciones Psicológicas (IIPsi-UNC-CONICET), Universidad Nacional de 12 Córdoba, Boulevard de la Reforma y Enfermera Gordillo s/n., 2do piso, Córdoba 5000, 13 Argentina 14 * corresponding author: [email protected] 15 16 Abstract 17 The Andean plateau is a small region of South America extending between northwest 18 Argentina, southwest Bolivia and northern Chile. -
Atacama Pacific Gold Corporation
TECHNICAL REPORT on the CERRO MARICUNGA GOLD PROJECT Region III CHILE prepared for ATACAMA PACIFIC GOLD CORPORATION 330 Bay Street, Suite 1210, Toronto, Ontario Canada M5H 2S8 October 7, 2011 Prepared By: Michael Easdon, Oregon Reg. Prof. Geologist Alcántara 1128, Depto. 905, Las Condes Santiago, Chile [email protected] TABLE OF CONTENTS 1.0 SUMMARY ........................................................................................................... 1 2.0 INTRODUCTION .................................................................................................. 5 3.0 RELIANCE ON OTHER EXPERTS ...................................................................... 7 4.0 PROPERTY DESCRIPTION AND LOCATION ..................................................... 8 5.0 ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY ............................................................................................... 13 6.0 HISTORY ........................................................................................................... 15 7.0 GEOLOGICAL SETTING AND MINERALIZATION ............................................ 15 7.1 PROPERTY GEOLOGY: ............................................................................. 16 8.0 DEPOSIT TYPE ................................................................................................. 33 9.0 EXPLORATION .................................................................................................. 34 10.0 DRILLING .......................................................................................................... -
Binational Study of the Transboundary San Pedro Aquifer
BINATIONAL STUDY OF THE TRANSBOUNDARY SAN PEDRO AQUIFER Final Report 2016 AUTHORITY This study was carried out by the United States and Mexico in accordance with resolution 6 of Minute 242 of the International Boundary and Water Commission, United States and Mexico (IBWC) entitled “Permanent and Definitive Solution to the International Problem of the Salinity of the Colorado River”, dated August 30, 1973; and the "Joint Report of the Principal Engineers Regarding the Joint Cooperative Process United States- Mexico for the Transboundary Aquifer Assessment Program”, dated August 19, 2009. FUNDING The funding for this study came from the United States Geological Survey Groundwater Resources Program and Transboundary Aquifer Assessment Program, the University of Arizona Water Resources Research Center and Technology Research and Initiative Fund, Mexico's National Water Commission, and the International Boundary and Water Commission, United States and Mexico. PARTICIPATING AGENCIES International Boundary and Water Commission United States and Mexico For Mexico: National Water Commission University of Sonora For the United States: United States Geological Survey The University of Arizona Water Resources Research Center Authors: J.B. Callegary, I. Minjárez Sosa, E.M. Tapia Villaseñor, P. dos Santos, R. Monreal Saavedra, F.J. Grijalva Noriega, A.K. Huth, F. Gray, C.A. Scott, L.A. Oroz Ramos, S.B. Megdal, M. Rangel Medina, J.M. Leenhouts Suggested Citation: Callegary, J.B., Minjárez Sosa, I., Tapia Villaseñor, E.M., dos Santos, P., Monreal Saavedra, R., Grijalva Noriega, F.J., Huth, A.K., Gray, F., Scott, C.A., Megdal, S.B., Oroz Ramos, L.A., Rangel Medina, M., Leenhouts, J.M., 2016, San Pedro River Aquifer Binational Report: International Boundary and Water Commission BINATIONAL STUDY GROUP For the International Boundary and Water Commission, United States and Mexico: - Edward Drusina, Commissioner, United States Section - John L. -
A Review of the Current State and Recent Changes of the Andean Cryosphere
feart-08-00099 June 20, 2020 Time: 19:44 # 1 REVIEW published: 23 June 2020 doi: 10.3389/feart.2020.00099 A Review of the Current State and Recent Changes of the Andean Cryosphere M. H. Masiokas1*, A. Rabatel2, A. Rivera3,4, L. Ruiz1, P. Pitte1, J. L. Ceballos5, G. Barcaza6, A. Soruco7, F. Bown8, E. Berthier9, I. Dussaillant9 and S. MacDonell10 1 Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA), CCT CONICET Mendoza, Mendoza, Argentina, 2 Univ. Grenoble Alpes, CNRS, IRD, Grenoble-INP, Institut des Géosciences de l’Environnement, Grenoble, France, 3 Departamento de Geografía, Universidad de Chile, Santiago, Chile, 4 Instituto de Conservación, Biodiversidad y Territorio, Universidad Austral de Chile, Valdivia, Chile, 5 Instituto de Hidrología, Meteorología y Estudios Ambientales (IDEAM), Bogotá, Colombia, 6 Instituto de Geografía, Pontificia Universidad Católica de Chile, Santiago, Chile, 7 Facultad de Ciencias Geológicas, Universidad Mayor de San Andrés, La Paz, Bolivia, 8 Tambo Austral Geoscience Consultants, Valdivia, Chile, 9 LEGOS, Université de Toulouse, CNES, CNRS, IRD, UPS, Toulouse, France, 10 Centro de Estudios Avanzados en Zonas Áridas (CEAZA), La Serena, Chile The Andes Cordillera contains the most diverse cryosphere on Earth, including extensive areas covered by seasonal snow, numerous tropical and extratropical glaciers, and many mountain permafrost landforms. Here, we review some recent advances in the study of the main components of the cryosphere in the Andes, and discuss the Edited by: changes observed in the seasonal snow and permanent ice masses of this region Bryan G. Mark, The Ohio State University, over the past decades. The open access and increasing availability of remote sensing United States products has produced a substantial improvement in our understanding of the current Reviewed by: state and recent changes of the Andean cryosphere, allowing an unprecedented detail Tom Holt, Aberystwyth University, in their identification and monitoring at local and regional scales. -
Boron and Other Trace Element Constraints on the Slab-Derived Component in Quaternary Volcanic Rocks from the Southern Volcanic Zone of the Andes
Geochemical Journal, Vol. 47, pp. 185 to 199, 2013 Boron and other trace element constraints on the slab-derived component in Quaternary volcanic rocks from the Southern Volcanic Zone of the Andes HIRONAO SHINJOE,1* YUJI ORIHASHI,2 JOSÉ A. NARANJO,3 DAIJI HIRATA,4 TOSHIAKI HASENAKA,5 TAKAAKI FUKUOKA,6 TAKASHI SANO7 and RYO ANMA8 1Tokyo Keizai University, Japan 2Earthquake Research Institute, The University of Tokyo, Japan 3Servicio Nacional de Geología y Minería, Chile 4Kanagawa Prefectural Museum of Natural History, Japan 5Department of Earth and Environmental Sciences, Graduate School of Science and Technology, Kumamoto University, Japan 6Department of Environment Systems, Faculty of Geo-environmental Science, Rissho University, Japan 7Department of Geology and Paleontology, National Museum of Nature and Science, Japan 8Integrative Environmental Sciences, Graduate School of Life and Environmental Sciences, Tsukuba University, Japan (Received April 18, 2012; Accepted December 25, 2012) We present a dataset for boron and other trace element contents obtained from samples from 13 volcanoes distributed along the Quaternary volcanic front of the Southern Volcanic Zone (SVZ) of the Chilean Andes. The dataset shows con- straints on the nature of slab-derived component to mantle source. Analyzed samples show large negative Nb and Ta anomalies, and enrichment of alkaline earth elements and Pb, which are features of typical island arc volcanic rocks. Boron contents of SVZ volcanic rocks range 2.3–125.5 ppm, exhibiting marked enrichment relative to N-MORB and OIB. Both the boron contents and B/Nb ratios of the volcanic rocks increase from the southern SVZ (SSVZ) to central SVZ (CSVZ). Fluid mobile/immobile element ratios (B/Nb, Ba/Nb, Pb/Nb, and K/Nb) are used to examine slab-derived com- ponent to mantle source. -
El Adoratorio Del Cerro El Potro: Arqueología De Alta Montaña En La Cordillera De Copiapó, Norte De Chile Ricardo Moyano1
El adoratorio del cerro El Potro: Arqueología de alta montaña en la cordillera de Copiapó, norte de Chile Ricardo Moyano1 D INTRODUCCIÓN Ricardo Moyano1 Resumen En los Andes Meridionales se considera a las montañas Se exponen los resultados del reconocimiento arqueológico de las como lugares sagrados por estar vinculadas con los ante- nacientes del río Los Helados y del cerro El Potro, en el valle de Copia- pó. El objetivo principal fue constatar evidencias descritas para la zona pasados y espíritus tutelares, los fenómenos metereoló- que dieran cuenta de una huaca prehispánica, como también definir la gicos y las actividades agrícolas y ganaderas, las riquezas orientación orográfica de la arquitectura del centro metalúrgico Viña del inframundo, así como con la suerte y salud de las per- del Cerro. Los resultados sugieren que existieron prácticas culturales sonas (Martínez 1976, 1983; Reinhard 1983). vinculadas con la tradición andina de adorar a las montañas, que incluyeron ceremonias públicas en Viña del Cerro, así como ceremonias restringidas en el cerro El Potro y sus inmediaciones. Esta dualidad El Tawantinsuyo habría incorporado la costumbre de ado- habría permitido manejar las relaciones de poder y reciprocidad entre rar a las montañas a su religión estatal como parte de los incas y los grupos locales, así como formar parte de ritos anuales de su estrategia de dominación. Este proceso involucró la fertilidad, base de la cadena productiva minero-metalúrgica del valle del subordinación de la mano de obra local para construir río Copiapó. o mejorar los tambos, plataformas y caminos; la utiliza- Palabras claves: cerro El Potro – Viña del Cerro – Tawantinsuyo – Copiapó. -
Dressing the Leader, Dressing the Ancestor: the Longue Durée in the South Central Andes Ann H
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Textile Society of America Symposium Proceedings Textile Society of America 2014 Dressing the Leader, Dressing the Ancestor: The longue durée in the South Central Andes Ann H. Peters University of Pennsylvania, [email protected] Follow this and additional works at: http://digitalcommons.unl.edu/tsaconf Part of the Art Practice Commons, and the Fiber, Textile, and Weaving Arts Commons Peters, Ann H., "Dressing the Leader, Dressing the Ancestor: The longue durée in the South Central Andes" (2014). Textile Society of America Symposium Proceedings. 945. http://digitalcommons.unl.edu/tsaconf/945 This Article is brought to you for free and open access by the Textile Society of America at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Textile Society of America Symposium Proceedings by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Dressing the Leader, Dressing the Ancestor: The longue durée in the South Central Andes Ann H. Peters The preservation and adornment of the dead in the South Central Andes can be traced over some twelve thousand years. The nature of social and political ancestry and its relationship to power change over time with the development of large-scale complex societies. These changes are reflected in the types of garments used to dress the outside of mortuary bundles and their references to socio-political roles and associations. Archaeology has barely begun to develop the analytic approaches to take advantage of textile analysis in order to reconstruct – or theorize – multifaceted identities, networks of social and political relationships, and production and exchange practices embedded in particular environments. -
Centro Comercial Metro
271,500 PARQUE 272,000 ELMER FAUCETT CENTRO COMERCIAL PQ. CAP. MANUEL METRO GALINDO (Auxiliar de la av. venezuela) Falco Manuel Tnte. Ca. Pje. Cap. Manuel Galindo Manuel Cap. Pje. Ca. Tnte. Juan Balcazar Ca. Teniente Eliseo Calmet San Nicolas San -U-RVp0DUtD0RUHOORV -U-RVp0DUtD0RUHOORV Pje. Bahia de Salinas de Bahia Pje. PQ. JOSE Pje. Bahia de Paracas PQ. DE LA MARIA Ca. Tnte. Enrique de Guimaraes PQ. Pje. Fogonero Isidro Alcibar Isidro Fogonero Pje. SOLIDARIDAD MORELLOS RESIDENCIAL PQ. Huarmey de Bahia Ca. FAUCETT FOGONERO 3MH%DKtDGHOD,QGHSHQGHQFLD 3MH%DKtD6DQ-XDQ Jr. Lautaro Jr. Pje. Pto. Lagunas 3MH%DKtDGH Pje. Bahia de Huacho de Bahia Pje. AV. PIO XII Pje. Bahia de Salinas de Bahia Pje. Ca. Fogonero Isidro Alcibar Isidro Fogonero Ca. AV. PIO XII Ca. Montecarlo Pje. Ampay Pje. Ca. Miguel Hidalgo Ca. Marinero Aparicio Robles Pje. Punta Zarate Punta Pje. Pje. Marinero Aparicio Robles PARQUE TRADICIONES DE RICARDO PALMA PQ. CAP. APARICIO ROBLES Lautaro Jr. Pje. Punta Sal -U-RVp0DUWL Pje. Punta Brava Punta Pje. PQ. PUNTA Ampay Ca. BOLSA BRAVA ESTACIONAMIENTO Pje. Punta Restin Jr. Cuauthemoc Jr. La Apacheta Jr. Cuauthemoc &D$xDTXLWR Pje. Punta Hermosa Punta Pje. Ca. Tutupaca Ca. Ca. Taquitahuana Ca. Camilo Carrillo Camilo Pje. Punta Balcones 3MH3XQWD3HxD1HJUD Jr. Paso de los Andes Jr. Paso de los Andes Jr.Pacamarca Pje. Punta Malpelo Ca.Huancauri AV. DE LOS INSURGENTES LOS DE AV. PQ. AV. ELMER FAUCETT PUNTA MALPELO Psj.Taquitahuana Jr. Capitan de Navio de Capitan Jr. 3MH3XQWD3DULxDV Ca. Quiquijana PQ. JOSE SANTOS CHOCANO Ca. Coropuna 8'665,500 Ca. Cap. de Navio German Stiglich Ca. -
Challenges in Ascertaining the Late Quaternary Tephrostratigraphy of Southernmost Chile and Argentina Stefan M
Challenges in ascertaining the late Quaternary tephrostratigraphy of southernmost Chile and Argentina 1 1 2 1 1 3 Stefan M. Lachowycz , Karen Fontijn , Victoria C. Smith , David M. Pyle , Tamsin A. Mather , José A. Naranjo [1] Department of Earth Sciences, University of Oxford, UK [2] Research Laboratory for Archaeology and the History of Art, University of Oxford, UK [3] Servicio Nacional de Geología y Minería, Santiago, Chile [email protected] # ## ! Overview Palaeoenvironmental archives 76°W 74°W 72°W 70°W 68°W 80°W 60°W 40°W Tephra preservation in palaeoenvironmental records Cha1 ! # 10°N ! Cha2 ! ! - The explosive eruption history and tephrostratigraphy in southernmost Chile/Argentina Minchinmávida Mic1 Issues with using tephra in palaeoenvironmental archives in this region to correlate records and constrain eruption parameters: and explosive eruption history ! # 0° ! Chaitén# Cor3 is significant for volcanic hazard assessment and as a tool to correlate and date reliably Corcovado# ! - 19 volcanic centres are thought to have been Cha2008 10°S Environment Physical preservation Chemical preservation Dating and record bias issues the many palaeoenvironmental archives here, but is currently poorly constrained. Yanteles# active in post-glacial times in southernmost # Yan1 Peat - Spatially and temporally variable - Al, Fe, alkali and alkali earth metals - Tephra layers are dispersed by root growth, 20°S 14 6 - We have reviewed the existing late Quaternary tephrostratigraphic record, and here # accumulation rates (F6, F7) ca use depth -
Contribución Al Conocimiento De La Zona Del Ojos Del Salado (Catamarca)
CONTRIBUCIÓN AL CONOCIMIENTO DE LA ZONA DEL OJOS DEL SALADO (CATAMARCA) A ntecedentes Si consultamos el trabajo de Pedro O. Sánchez 1 los primeros que ievantaron mapas de la zona fueron Alcides D ’Orbigny (1 8 2 6 -3 3 ) ; José Ballivián, mandado por Bolivia (1843) ; Hoogsgaard, por el Perú (1873- 74) ; Amado Pissis, encargado por Chile de estudiar el relieve de la Repú blica desde 1848, quien luego trabajó con Mariano Mugía, boliviano. En 1883, dice Sánchez, Chile mandó levantar una carta a Francisco San R o mán, Santiago Muñoz, Alejandro Chadwick y Abelardo Pizarro, comisión que trabajó con exactitud y sembró la Puna de sugestivos nombres en ho menaje a los científicos que la visitaron: cordilleras D ’Orbigny, Claudio Gay, Domeyko, sierras Gorbea, Barros Arana, monte Pissis, altiplanicie F*hilippi, etc. Alejandro Bertrand, casi en la misma época, se dedicó a la Puna y a sus altas cumbres y publicó Memoria sobre el desierto de A ta- cama y sus regiones limítrofes (1 8 8 4 ). Para su trabajo se valió de cartas anteriores, especialmente las de San Román, Hugo Reck, boliviano, ( 1860- 1863) y la de Brackebusch, mandado por Argentina. El Tnte. de Navio Vicente Montes 1 2 fue encargado por el perito argentino, en el pleito de límites con Chile, de estudiar la región montañosa entre los paralelos 26 y 28 a fin de determinar con precisión qué se debía considerar como cordillera de Los Andes El 29 de abril de 1892 3 con vinieron los peritos en que una comisión mixta iniciaría la demarcación desde el Portezuelo de San Francisco hacia el sur, integrada por Julio Díaz, Luis Dellepiane, Fernando Dousset (Argentina) y Alejandro Bertrand, Aníbal Contreras y Alvaro Donoso (C hile). -
Glacier Inventory and Recent Glacier Variations in the Andes of Chile, South America
Annals of Glaciology 58(75pt2) 2017 doi: 10.1017/aog.2017.28 166 © The Author(s) 2017. This is an Open Access article, distributed under the terms of the Creative Commons Attribution-NonCommercial-NoDerivatives licence (http://creativecommons.org/licenses/by-nc-nd/4.0/), which permits non-commercial re-use, distribution, and reproduction in any medium, provided the original work is unaltered and is properly cited. The written permission of Cambridge University Press must be obtained for commercial re-use or in order to create a derivative work. Glacier inventory and recent glacier variations in the Andes of Chile, South America Gonzalo BARCAZA,1 Samuel U. NUSSBAUMER,2,3 Guillermo TAPIA,1 Javier VALDÉS,1 Juan-Luis GARCÍA,4 Yohan VIDELA,5 Amapola ALBORNOZ,6 Víctor ARIAS7 1Dirección General de Aguas, Ministerio de Obras Públicas, Santiago, Chile. E-mail: [email protected] 2Department of Geography, University of Zurich, Zurich, Switzerland 3Department of Geosciences, University of Fribourg, Fribourg, Switzerland 4Institute of Geography, Pontificia Universidad Católica de Chile, Santiago, Chile 5Centre for Hydrology, University of Saskatchewan, Saskatoon, Canada 6Department of Geology, University of Concepción, Concepción, Chile 7Department of Geology, University of Chile, Santiago, Chile ABSTRACT. The first satellite-derived inventory of glaciers and rock glaciers in Chile, created from Landsat TM/ETM+ images spanning between 2000 and 2003 using a semi-automated procedure, is pre- sented in a single standardized format. Large glacierized areas in the Altiplano, Palena Province and the periphery of the Patagonian icefields are inventoried. The Chilean glacierized area is 23 708 ± 1185 km2, including ∼3200 km2 of both debris-covered glaciers and rock glaciers.