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512 INDEX 4WD Tours Iquique 198 Porvenir 411-12 Uyuni (Bol) 215 A
© Lonely Planet Publications 512 Index Aldea de Tulor 220 Museo Municipal de Bellas Artes ABBREVIATIONS alerce 65, 346 (Viña del Mar) 135 Arg Argentina Allende, Salvador 36, 37-8, 92 Museo Nacional de Bellas Artes Bol Bolivia alpacas 64 (Santiago) 87 Altiplano lakes 215 arts 47-52 4WD tours Ana Kai Tangata 455 Atacama Desert 21, 62, 207, 216 Iquique 198 Ana Te Pahu 454 Atacameño peoples 31, 46, 175, 220 Porvenir 411-12 Ancud 323-7, 325 Atoca 185 Uyuni (Bol) 215 Angol 171-2 ATMs 469 animals 63-4, 432, see also individual Ayquina 222 A species Aymara peoples 31, 45, 46, 181, 187, accommodations 460-2, see also Antarctica 421, 422 190, 191 individual locations Antillanca 300 language 497-8 Antofagasta 223-7, 224 B Achao 331-2 aquaculture 69, 315 Bachelet, Michelle 42, 43 activities 23, 70-5, 462-3, see also araucaria 65, 260, 272, 286 Bahía Inglesa 235 individual activities archaeological sites, see geoglyphs, Bahía Tierras Blancas 437 addresses 463 petroglyphs Baños Morales 119 Aguas Calientes 300 Archipiélago Juan Fernández 429- Baquedano 207 ahu 457 38, 431 bargaining 471 Ahu Akahanga 456 architecture 51 bars 54 Ahu Akapu 446 area codes 472, see also inside front bathrooms 472 INDEX Ahu Akivi 454-5 cover beaches Ahu Ature Huki 459 Arica 177-85, 179 Arica 180 Ahu Hanga Tetenga 456 art galleries & art museums Bahía Inglesa 235 Ahu Nau Nau 459 Bodegón Cultural 262 Concón 139 Ahu Riata 446 Casa del Arte Diego Rivera 315 Coquimbo 251-2 Ahu Tahai 446 Centro Cultural Matucana 91 Easter Island 446, 458-9, 459 Ahu Tautira 446 Centro Cultural Palacio -
Download Itinerary
PATAGONIA - SANTIAGO TO LA PAZ TRIP CODE LATSSALP DURATION 13 Days LOCATIONS Chile, Bolivia, Patagonia INTRODUCTION Travel to South America and set off on an unforgettable adventure through the soaring Andes, meeting friendly locals and discovering the rich culture and breathtaking scenery of this remarkable region. Starting in Chile's vibrant Santiago surrounded by an extraordinary set of snow-capped Andean mountains, travel to the expansive San Pedro Atacama and Salar de Uyuni where you will enjoy surreal landscapes and abundant wildlife, including wild vicunas and multi coloured lakes filled with flamingos. Finish the adventure in colourful La Paz. This amazing trip is the perfect way to experience the best of this spectacular region. ITINERARY DAY 1: Arrival transfer in Santiago On arrival at Santiago Airport, please make your way through Customs and Immigration and only exit from the green doors marked 'Meeting Point’. Our representative will be holding a sign with your name on it and waiting for you outside this exit. Please only make contact with our representative. This service includes a driver and local English speaking guide who will provide you with any useful information needed for your stay. Copyright Chimu Adventures. All rights reserved 2020. Chimu Adventures PTY LTD PATAGONIA - SANTIAGO TO LA PAZ DAY 1: Santiago de Chile TRIP CODE Santiago, Chile’s capital and largest city, lies in a valley surrounded by the snow-capped mountains LATSSALP of the Andes and the Chilean Coastal Range. Founded in 1541, Santiago has been Chile’s DURATION capital since colonial times. It is a vibrant and cosmopolitan city and although it features many colonial buildings, it has grown into a modern 13 Days metropolis and the cultural centre of the country. -
Hydrothermal Alteration, Fumarolic Deposits and Fluids from Lastarria Volcanic Complex: a Multidisciplinary Study
Andean Geology 42 (3): 166-196. May, 2016 Andean Geology doi: 10.5027/andgeoV43n2-a02 www.andeangeology.cl Hydrothermal alteration, fumarolic deposits and fluids from Lastarria Volcanic Complex: A multidisciplinary study *Felipe Aguilera1, Susana Layana2, Augusto Rodríguez-Díaz3, Cristóbal González2, Julio Cortés4, Manuel Inostroza2 1 Departamento de Ciencias Geológicas, Universidad Católica del Norte, Avda. Angamos 0610, Antofagasta, Chile. [email protected] 2 Programa de Doctorado en Ciencias mención Geología, Universidad Católica del Norte, Avda. Angamos 0610, Antofagasta, Chile. [email protected]; [email protected]; [email protected] 3 Instituto de Geofísica, Universidad Nacional Autónoma de México, Ciudad Universitaria, Delegación Coyoacán, 04150 México D.F., México. [email protected] 4 Consultor Independiente, Las Docas 4420, La Serena, Chile. [email protected] * Corresponding Author: [email protected] ABSTRACT. A multidisciplinary study that includes processing of Landsat ETM+ satellite images, chemistry of gas condensed, mineralogy and chemistry of fumarolic deposits, and fluid inclusion data from native sulphur deposits, has been carried out in the Lastarria Volcanic Complex (LVC) with the objective to determine the distribution and charac- teristics of hydrothermal alteration zones and to establish the relations between gas chemistry and fumarolic deposits. Satellite image processing shows the presence of four hydrothermal alteration zones, characterized by a mineral -
El Patrimonio Natural De Chile: Flora Y Fauna
Actividad Semanal Historia, Geografía y Ciencias Sociales 2° Año Básico Docente de Asignatura: Jacqueline Madrid Orellana OA (OA 5) Reconocer diversas expresiones del patrimonio cultural del país y de la región, tales como manifestaciones artísticas, tradiciones folclóricas, leyendas. Objetivo semanal Identificar las expresiones del patrimonio natural de Chile: flora y fauna. Fechas Semana del 09 al 13 de Noviembre del 2020 Unidad N 4: Tradiciones, costumbres y patrimonio chileno Asignatura: Historia, Geografía y Ciencias Sociales Curso: 2º Básico Mes: Noviembre Apuntes 19 “Hola queridos estudiantes y familia” Bienvenidos a nuestra clase de Historia. Esta semana seguiremos aprendiendo y seguir con ese maravilloso entusiasmo y esfuerzo. A continuación, te mostrare lo que realizaremos durante la clase de Historia Ruta de aprendizaje Recordar contenido Leer y comprender Responder preguntas de la clase anterior información Practicar Realizar actividad Conoces estos lugares La moneda Moais de isla de Mercado Central Ascensor de Valparaíso Son parte de nuestro patrimonio cultural Sabías que el patrimonio cultural es un conjunto de elementos que son relevantes para la cultura de nuestro pueblo. Como, por ejemplo: los museos, edificios, costumbres, comidas y bailes. Bienes culturales valiosos que heredamos de nuestros antepasados que nos permiten conocer nuestra historia y preservarla para el futuro. El patrimonio cultural puede ser tangible e intangible. Tangible: Visibles como: edificios históricos, iglesias, obras de arte, sitios arqueológicos, fotografías, zonas típicas y monumentos. Intangible: Son los valores y expresiones que caracterizan a un pueblo o nación. Como, por ejemplo: Leyendas, tradiciones, fiestas típicas, refranes, canciones, creencias y música. Comencemos Sabías que… El patrimonio natural: está constituido por monumentos naturales construidos por formaciones físicas y biológicas, es decir, estas fueron creadas poco a poco a lo largo del tiempo por la naturaleza. -
The Volcanic Ash Soils of Chile
' I EXPANDED PROGRAM OF TECHNICAL ASSISTANCE No. 2017 Report to the Government of CHILE THE VOLCANIC ASH SOILS OF CHILE FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS ROMEM965 -"'^ .Y--~ - -V^^-.. -r~ ' y Report No. 2017 Report CHT/TE/LA Scanned from original by ISRIC - World Soil Information, as ICSU World Data Centre for Soils. The purpose is to make a safe depository for endangered documents and to make the accrued information available for consultation, following Fair Use Guidelines. Every effort is taken to respect Copyright of the materials within the archives where the identification of the Copyright holder is clear and, where feasible, to contact the originators. For questions please contact [email protected] indicating the item reference number concerned. REPORT TO THE GOVERNMENT OP CHILE on THE VOLCANIC ASH SOILS OP CHILE Charles A. Wright POOL ANL AGRICULTURE ORGANIZATION OP THE UNITEL NATIONS ROME, 1965 266I7/C 51 iß - iii - TABLE OP CONTENTS Page INTRODUCTION 1 ACKNOWLEDGEMENTS 1 RECOMMENDATIONS 1 BACKGROUND INFORMATION 3 The nature and composition of volcanic landscapes 3 Vbloanio ash as a soil forming parent material 5 The distribution of voloanic ash soils in Chile 7 Nomenclature used in this report 11 A. ANDOSOLS OF CHILE» GENERAL CHARACTERISTICS, FORMATIVE ENVIRONMENT, AND MAIN KINDS OF SOIL 11 1. TRUMAO SOILS 11 General characteristics 11 The formative environment 13 ÈS (i) Climate 13 (ii) Topography 13 (iii) Parent materials 13 (iv) Natural plant cover 14 (o) The main kinds of trumao soils ' 14 2. NADI SOILS 16 General characteristics 16 The formative environment 16 tö (i) Climat* 16 (ii) Topograph? and parent materials 17 (iii) Natural plant cover 18 B. -
Latitud 90 Get Inspired.Pdf
Dear reader, To Latitud 90, travelling is a learning experience that transforms people; it is because of this that we developed this information guide about inspiring Chile, to give you the chance to encounter the places, people and traditions in most encompassing and comfortable way, while always maintaining care for the environment. Chile offers a lot do and this catalogue serves as a guide to inform you about exciting, adventurous, unique, cultural and entertaining activities to do around this beautiful country, to show the most diverse and unique Chile, its contrasts, the fascinating and it’s remoteness. Due to the fact that Chile is a country known for its long coastline of approximately 4300 km, there are some extremely varying climates, landscapes, cultures and natures to explore in the country and very different geographical parts of the country; North, Center, South, Patagonia and Islands. Furthermore, there is also Wine Routes all around the country, plus a small chapter about Chilean festivities. Moreover, you will find the most important general information about Chile, and tips for travellers to make your visit Please enjoy reading further and get inspired with this beautiful country… The Great North The far north of Chile shares the border with Peru and Bolivia, and it’s known for being the driest desert in the world. Covering an area of 181.300 square kilometers, the Atacama Desert enclose to the East by the main chain of the Andes Mountain, while to the west lies a secondary mountain range called Cordillera de la Costa, this is a natural wall between the central part of the continent and the Pacific Ocean; large Volcanoes dominate the landscape some of them have been inactive since many years while some still present volcanic activity. -
Full-Text PDF (Final Published Version)
Pritchard, M. E., de Silva, S. L., Michelfelder, G., Zandt, G., McNutt, S. R., Gottsmann, J., West, M. E., Blundy, J., Christensen, D. H., Finnegan, N. J., Minaya, E., Sparks, R. S. J., Sunagua, M., Unsworth, M. J., Alvizuri, C., Comeau, M. J., del Potro, R., Díaz, D., Diez, M., ... Ward, K. M. (2018). Synthesis: PLUTONS: Investigating the relationship between pluton growth and volcanism in the Central Andes. Geosphere, 14(3), 954-982. https://doi.org/10.1130/GES01578.1 Publisher's PDF, also known as Version of record License (if available): CC BY-NC Link to published version (if available): 10.1130/GES01578.1 Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via Geo Science World at https://doi.org/10.1130/GES01578.1 . Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Research Paper THEMED ISSUE: PLUTONS: Investigating the Relationship between Pluton Growth and Volcanism in the Central Andes GEOSPHERE Synthesis: PLUTONS: Investigating the relationship between pluton growth and volcanism in the Central Andes GEOSPHERE; v. 14, no. 3 M.E. Pritchard1,2, S.L. de Silva3, G. Michelfelder4, G. Zandt5, S.R. McNutt6, J. Gottsmann2, M.E. West7, J. Blundy2, D.H. -
Nota Sobre Neruda
Una nota sobre Pablo Neruda Para el Club de Lectura del Politécnico Grancolombiano 1904 Neftalí Ricardo Reyes Basoalto (Pablo Neruda) nace el 12 de julio, en Parral, Chile, hijo de Rosa Basoalto de Reyes y de José del Carmen Reyes Morales. Neruda pierde a su madre cuando tiene un mes de edad y crece huérfano hasta que don José del Carmen contrae segundas nupcias dos años después. 1906 Don José del Carmen se traslada a Temuco y se casa en segundas nupcias con doña Trinidad Candia Marverde. Neruda fue llevado a Temuco unos pocos años después. _______________________________________________________ Neruda le inventa a la madrastra el nombre de mamadre. _______________________________________________________ 1910 Pablo Neruda ingresa al Liceo de Hombres de Temuco, y termina el 6º año de humanidades en 1920. _______________________________________________________ Mi primer poema [Confieso que he vivido Memorias] Muchas veces me he preguntado cuándo escribí mi primer poema, cuando nació en mí la poesía. Trataré de recordarlo. Muy atrás en mi infancia y habiendo apenas aprendido a escribir, sentí una vez una intensa emoción y tracé unas cuantas palabras semirrimadas, pero extrañas a mí, diferentes del lenguaje diario. Las puse en limpio en un papel, preso de una ansiedad profunda, de un sentimiento hasta entonces desconocido, especie de angustia y de tristeza. Era un poema dedicado a mi madre, es decir, a la que conocí por tal, a la angelical madrastra cuya suave sombra protegió toda mi infancia. Completamente incapaz de juzgar mi primera producción, se la llevé a mis padres. Ellos estaban en el comedor, sumergidos en una de esas conversaciones en voz baja que dividen más que un río el mundo de los niños y el de los adultos. -
Effects of Volcanism, Crustal Thickness, and Large Scale Faulting on the He Isotope Signatures of Geothermal Systems in Chile
PROCEEDINGS, Thirty-Eighth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, February 11-13, 2013 SGP-TR-198 EFFECTS OF VOLCANISM, CRUSTAL THICKNESS, AND LARGE SCALE FAULTING ON THE HE ISOTOPE SIGNATURES OF GEOTHERMAL SYSTEMS IN CHILE Patrick F. DOBSON1, B. Mack KENNEDY1, Martin REICH2, Pablo SANCHEZ2, and Diego MORATA2 1Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA 94720 USA 2Departamento de Geología y Centro de Excelencia en Geotermia de los Andes, Universidad de Chile, Santiago, CHILE [email protected] agree with previously published results for the ABSTRACT Chilean Andes. The Chilean cordillera provides a unique geologic INTRODUCTION setting to evaluate the influence of volcanism, crustal thickness, and large scale faulting on fluid Measurement of 3He/4He in geothermal water and gas geochemistry in geothermal systems. In the Central samples has been used to guide geothermal Volcanic Zone (CVZ) of the Andes in the northern exploration efforts (e.g., Torgersen and Jenkins, part of Chile, the continental crust is quite thick (50- 1982; Welhan et al., 1988) Elevated 3He/4He ratios 70 km) and old (Mesozoic to Paleozoic), whereas the (R/Ra values greater than ~0.1) have been interpreted Southern Volcanic Zone (SVZ) in central Chile has to indicate a mantle influence on the He isotopic thinner (60-40 km) and younger (Cenozoic to composition, and may indicate that igneous intrusions Mesozoic) crust. In the SVZ, the Liquiñe-Ofqui Fault provide the primary heat source for the associated System, a major intra-arc transpressional dextral geothermal fluids. Studies of helium isotope strike-slip fault system which controls the magmatic compositions of geothermal fluids collected from activity from 38°S to 47°S, provides the opportunity wells, hot springs and fumaroles within the Basin and to evaluate the effects of regional faulting on Range province of the western US (Kennedy and van geothermal fluid chemistry. -
Taxonomic Revision of the Chilean Puya Species (Puyoideae
Taxonomic revision of the Chilean Puya species (Puyoideae, Bromeliaceae), with special notes on the Puya alpestris-Puya berteroniana species complex Author(s): Georg Zizka, Julio V. Schneider, Katharina Schulte and Patricio Novoa Source: Brittonia , 1 December 2013, Vol. 65, No. 4 (1 December 2013), pp. 387-407 Published by: Springer on behalf of the New York Botanical Garden Press Stable URL: https://www.jstor.org/stable/24692658 JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at https://about.jstor.org/terms New York Botanical Garden Press and Springer are collaborating with JSTOR to digitize, preserve and extend access to Brittonia This content downloaded from 146.244.165.8 on Sun, 13 Dec 2020 04:26:58 UTC All use subject to https://about.jstor.org/terms Taxonomic revision of the Chilean Puya species (Puyoideae, Bromeliaceae), with special notes on the Puya alpestris-Puya berteroniana species complex Georg Zizka1'2, Julio V. Schneider1'2, Katharina Schulte3, and Patricio Novoa4 1 Botanik und Molekulare Evolutionsforschung, Senckenberg Gesellschaft für Naturforschung and Johann Wolfgang Goethe-Universität, Senckenberganlage 25, 60325, Frankfurt am Main, Germany; e-mail: [email protected]; e-mail: [email protected] 2 Biodiversity and Climate Research Center (BIK-F), Senckenberganlage 25, 60325, Frankfurt am Main, Germany 3 Australian Tropical Herbarium and Tropical Biodiversity and Climate Change Centre, James Cook University, PO Box 6811, Caims, QLD 4870, Australia; e-mail: [email protected] 4 Jardin Botânico Nacional, Camino El Olivar 305, El Salto, Vina del Mar, Chile Abstract. -
“Walking Around” Pablo Neruda I. Características De La Poesía De
“Walking Around” Pablo Neruda I. Características de la poesía de Neruda del período poemario Residencia en la tierra. Mencione, además, algunos datos biográficos del poeta y algunas de sus obras: A. Características de la poesía de Neruda del período poemario Residencia en la tierra: Posee todos los atributos que caracterizan a la ruptura vanguardista. Surge íntimamente ligado a la noción de crisis generalizada y, promueve un corte radical con el pasado. Surge íntimamente ligado a la noción de crisis generalizada y, promueve un corte radical con el pasado. Participa en la renovación profunda de las concepciones, las conductas y las realizaciones artísticas. Cambio de percepto y cambio de precepto van a la par. Neruda acomete una revolución instrumental porque promueve una revolución mental. Su arte impugna la imagen tradicional del mundo, contraviene sobre todo la altivez teocéntrica y la vanidad antropocéntrica del humanismo idealista; e impugna el mundo de la imagen: la mímesis realista, la visión perspectivista, la representación progresiva y cohesiva, la figuración simétrico-extensiva, la composición concertante, la expresión estilizada, el arte de la totalidad armónica. Cambio de mentalidad que conlleva una crisis raigal de valores. Refleja ese estallido de los marcos familiares, de vida y de referencia que trastorna la estabilidad del orden preindustrial (comarcano, aldeano, rural, artesanal), que trastoca el mundo solariego de las relaciones personalizadas, las solidaridades 1 | “ Walking Around ” seculares de la comunidad local sometidas ahora al embate de un proceso que masifica y uniformiza aceleradamente. Neruda no adhiere a la modernolatría futurista, no participa de la vanguardia eufórica aquella que alaba las conquistas del mundo moderno, la que asume los imperativos del programa tecnológico: avance permanente, incesante renovación de procedimientos y de productos, constante suplantación de lo objetual, perpetua modificación nocional. -
Glacier Runoff Variations Since 1955 in the Maipo River Basin
https://doi.org/10.5194/tc-2019-233 Preprint. Discussion started: 5 November 2019 c Author(s) 2019. CC BY 4.0 License. Glacier runoff variations since 1955 in the Maipo River Basin, semiarid Andes of central Chile Álvaro Ayala1,2, David Farías-Barahona3, Matthias Huss1,2,4, Francesca Pellicciotti2,5, James McPhee6,7, Daniel Farinotti1,2 5 1Laboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zurich, Zurich, 8093, Switzerland. 2Swiss Federal Institute for Forest, Snow and Landscape Research, Birmensdorf, 8903, Switzerland. 3Institut für Geographie, Friedrich-Alexander-Universität Erlangen-Nürnberg, Erlangen, 91058, Germany 4Department of Geosciences, University of Fribourg, Fribourg, 1700, Switzerland 5Department of Geography, Northumbria University, Newcastle, NE1 8ST, UK. 10 6Department of Civil Engineering, University of Chile, Santiago, 8370449, Chile. 7Advanced Mining Technology Centre (AMTC), University of Chile, Santiago, 8370451, Chile. Correspondence to: Alvaro Ayala ([email protected]), now at Centre for Advanced Studies in Arid Zones (CEAZA) Abstract (max 250 words). As glaciers adjust their size in response to climate variations, long-term changes in meltwater production can be expected, affecting the local availability of water resources. We investigate glacier runoff in the period 15 1955-2016 in the Maipo River Basin (4 843 km2), semiarid Andes of Chile. The basin contains more than 800 glaciers covering 378 km2 (inventoried in 2000). We model the mass balance and runoff contribution of 26 glaciers with the physically-oriented and fully-distributed TOPKAPI-ETH glacio-hydrological model, and extrapolate the results to the entire basin. TOPKAPI- ETH is run using several glaciological and meteorological datasets, and its results are evaluated against streamflow records, remotely-sensed snow cover and geodetic mass balances for the periods 1955-2000 and 2000-2013.