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Vistas of Bolivia
13 days 1:31 24-07-2021 We are the UK’s No.1 specialist in travel to Latin As our name suggests, we are single-minded America and have been creating award-winning about Latin America. This is what sets us apart holidays to every corner of the region for over four from other travel companies – and what allows us decades; we pride ourselves on being the most to offer you not just a holiday but the opportunity to knowledgeable people there are when it comes to experience something extraordinary on inspiring travel to Central and South America and journeys throughout Mexico, Central and South passionate about it too. America. A passion for the region runs Fully bonded and licensed Our insider knowledge helps through all we do you go beyond the guidebooks ATOL-protected All our Consultants have lived or We hand-pick hotels with travelled extensively in Latin On your side when it matters character and the most America rewarding excursions Book with confidence, knowing Up-to-the-minute knowledge every penny is secure Let us show you the Latin underpinned by 40 years' America we know and love experience 1:31 24-07-2021 1:31 24-07-2021 Bolivia is the Latin America of your imagination. It’s a country of outsized wilderness landscapes, of rock-falls blocking cliff-hugging dirt roads, boozy fiestas, far-flung weaving villages, and age-weathered colonnades. It’s where otherworldly features such as sun-blistered salt pans sit within wind-blasted plains, pinpricked by ice- coated Andean spires. This holiday fizzes with adventure: add to the above the sapphire waters of Lake Titicaca, the panoramic cable cars of La Paz and the remote trail tracing the route of Che Guevara’s last stand: we’ve created an innovative group tour trip where surprises lurk round every corner. -
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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. -
Salt Lakes and Pans
SCIENCE FOCUS: Salt Lakes and Pans Ancient Seas, Modern Images SeaWiFS image of the western United States. The features of interest that that will be discussed in this Science Focus! article are labeled on the large image on the next page. (Other features and landmarks are also labeled.) It should be no surprise to be informed that the Sea-viewing Wide Field-of-view Sensor (SeaWiFS) was designed to observe the oceans. Other articles in the Science Focus! series have discussed various oceanographic applications of SeaWiFS data. However, this article discusses geological features that indicate the presence of seas that existed in Earth's paleohistory which can be discerned in SeaWiFS imagery. SeaWiFS image of the western United States. Great Salt Lake and Lake Bonneville The Great Salt Lake is the remnant of ancient Lake Bonneville, which gave the Bonneville Salt Flats their name. Geologists estimate that Lake Bonneville existed between 23,000 and 12,000 years ago, during the last glacial period. Lake Bonneville's existence ended abruptly when the waters of the lake began to drain rapidly through Red Rock Pass in southern Idaho into the Snake River system (see "Lake Bonneville's Flood" link below). As the Earth's climate warmed and became drier, the remaining water in Lake Bonneville evaporated, leaving the highly saline waters of the Great Salt Lake. The reason for the high concentration of dissolved minerals in the Great Salt Lake is due to the fact that it is a "terminal basin" lake; water than enters the lake from streams and rivers can only leave by evaporation. -
From the Atacama Desert to the Amazon Jungle
GROUP TOUR HIE 2117 PRICE PER PERSON FROM THE ATACAMA DESERT IN DOUBLE OCCUPANCY from USD 3.965.- TO THE AMAZON JUNGLE EUR 3.276.- WITH EXTENSION TO CUSCO AND MACHU PICCHU TOUR DATES 2021 23 days - 22 nights August 13 - September 4 Two of the most imposing scenarios in the Americas are the Atacama Desert and the Amazon Jungle. The first is the most arid non-polar desert on Earth, with an approximate area of 105,000 INCLUSIONS km2 that extends in northern Chile and is bounded by the Pacific Ocean and the Andes mountain Local flights Santiago- Calama, Sucre-La Paz, La range. Some institutions consider its extension to the Peruvian coastal area; as well as the puna Paz-Rurrenabaque-La Paz and Cuzco-Lima in located on the 3500 meters above sea level that includes part of northern Argentina and South- economy class Sit-in basis program up to 15 pax. Minibus or West Bolivia. The Amazon Jungle is the largest rainforest in the world with an area of 7 million private van on request. km2 spread among Brazil that has the most, Bolivia, Colombia, Venezuela, and Ecuador. It 22 Hotel nights including Breakfast develops around the Amazonas river and its river basin. It has also been declared one of the seven Meal plan: HALFBOARD natural wonders of the world. All transfers and excursions as mentioned in the program. Therefore, we have planned this route in order to make you known two wonders of nature that Local guides in Spanish for all the excursions exceed expectations. mentioned in the program We start our trip in Santiago de Chile with visits that includes tasting of the best wines of the All entrance fees to national parks and excursions. -
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. -
Chile & Easter Island 9
©Lonely Planet Publications Pty Ltd “All you’ve got to do is decide to go and the hardest part is over. So go!” TONY WHEELER, COFOUNDER – LONELY PLANET Get the right guides for your trip PAGE PLAN YOUR PLANNING TOOL KIT 2 Photos, itineraries, lists and suggestions YOUR TRIP to help you put together your perfect trip Welcome to Chile ........... 2 Map .................................. 4 20 Top Experiences ....... 6 Welcome to Chile Need to Know ................. 16 If You Like ........................ 18 COUNTRY • The original Month by Month ............. 21 • Comprehensive • AdventurousAdventu Itineraries ........................ 23 (p ) g Artes (Beautiful Art) – says it all. Fan À ne arts can spend the day admiring works at the Museo Nacional de Bel and the Museo de Arte Contemporá housed in the stately Palacio de Bell Chile Outdoors ............... 28 before checking out edgy modern ph and sculpture at the nearby Museo d Meet A LandVisuales. of Along the way, take stayeda brea kintact for so long. The very human Extremes several sidewalk cafes along thequest co bfor development could imperil these pedestrian streets. Palacio detreasures Bellas A sooner than we think. For now, Travel with Children ....... 33 20Preposterously thin and unreasonably Chile guards parts of our planet that re- ong, Chile stretches from the belly of main the most pristine, and they shouldn’t outh America toParque its foot, reaching Nacional from be To missed.r he driest desert delon earth Paine to vast southern TOP lacial À elds. It’s nature on a symphonic La Buena Onda Some rites of passage never los EXPERIENCEScale. Diverse landscapes unfurl over a In Chile, close borders foster intimacy. -
Vita Singer June 2021
Brad S. Singer June, 2021 Professor http://geoscience.wisc.edu/geoscience/people/faculty/brad-singer/ Department of Geoscience WiscAr Lab: https://geochronology.geoscience.wisc.edu University of Wisconsin-Madison [email protected] 1215 W. Dayton Street tel: +1 608 265 8650 Madison, WI 53706 EDUCATION 1990 Ph.D. Geology, University of Wyoming 1985 M.S. Geology, University of New Mexico 1983 B.A. Geological Sciences, University of California, Santa Barbara PROFESSIONAL APPOINTMENTS 2020- Chair, Department of Geoscience, University of Wisconsin-Madison 2017 summer Visiting Professor, Tohoku University, Sendai, Japan 2015 summer Visiting Professor, Earth Observatory of Singapore, Nanyang Technological University 2011-2014 Chair, Department of Geoscience, University of Wisconsin-Madison 2006-present Professor, Department of Geoscience, University of Wisconsin-Madison 2006 Visiting Scientist, Laboratoire des Sciences du Climat et de l'Environnement, Gif sur Yvette, France 2003-2006 Associate Professor, Department of Geoscience, University of Wisconsin-Madison 1999-2003 Assistant Professor, Department of Geoscience, University of Wisconsin-Madison 1993-1998 Maître Assistant, Dépt. de Minéralogie, Université de Genève, Genève, Switzerland 1991-1993 Research Fellow, Dept. of Geological Sciences, Southern Methodist University, Dallas, TX 1990-1991 Visiting Assistant Professor, Dept. of Geological Sciences, Univ. of Michigan, Ann Arbor, MI HONORS and AWARDS 2019 Vilas Distinguished Achievement Professor, UW-Madison 2019 Fellow of the Geological Society -
Impact of the 1960 Major Subduction Earthquake in Northern Patagonia (Chile, Argentina)
ARTICLE IN PRESS Quaternary International 158 (2006) 58–71 Impact of the 1960 major subduction earthquake in Northern Patagonia (Chile, Argentina) Emmanuel Chaprona,b,Ã, Daniel Arizteguic, Sandor Mulsowd, Gustavo Villarosae, Mario Pinod, Valeria Outese, Etienne Juvignie´f, Ernesto Crivellie aRenard Centre of Marine Geology, Ghent University, Ghent, Belgium bGeological Institute, ETH Zentrum, Zu¨rich, Switzerland cInstitute F.A. Forel and Department of Geology and Paleontology, University of Geneva, Geneva, Switzerland dInstituto de Geociencias, Universidad Austral de Chile, Valdivia, Chile eCentro Regional Universitario Bariloche, Universidad Nacional del Comahue, Bariloche, Argentina fPhysical Geography,Universite´ de Lie`ge, Lie`ge, Belgium Available online 7 July 2006 Abstract The recent sedimentation processes in four contrasting lacustrine and marine basins of Northern Patagonia are documented by high- resolution seismic reflection profiling and short cores at selected sites in deep lacustrine basins. The regional correlation of the cores is provided by the combination of 137Cs dating in lakes Puyehue (Chile) and Frı´as (Argentina), and by the identification of Cordon Caulle 1921–22 and 1960 tephras in lakes Puyehue and Nahuel Huapi (Argentina) and in their catchment areas. This event stratigraphy allows correlation of the formation of striking sedimentary events in these basins with the consequences of the May–June 1960 earthquakes and the induced Cordon Caulle eruption along the Liquin˜e-Ofqui Fault Zone (LOFZ) in the Andes. While this catastrophe induced a major hyperpycnal flood deposit of ca. 3 Â 106 m3 in the proximal basin of Lago Puyehue, it only triggered an unusual organic rich layer in the proximal basin of Lago Frı´as, as well as destructive waves and a large sub-aqueous slide in the distal basin of Lago Nahuel Huapi. -
Geographical Data of Chilean Lizards and Snakes in the Museo Nacional De Historia Natural Santiago, Chile
GEOGRAPHICAL DATA OF CHILEAN LIZARDS AND SNAKES IN THE MUSEO NACIONAL DE HISTORIA NATURAL SANTIAGO, CHILE HERMAN NUNEZ Seccion Zoologia Museo Nacional de Historia Natural SMITHSONIAN HERPETOLOGICAL INFORMATION SERVICE NO. 91 1992 SMITHSONIAN HERPETOLOGICAL INFORMATION SERVICE The SHIS series publishes and distributes translations, bibliographies, indices, and similar items judged useful to individuals interested in the biology of amphibians and reptiles, but unlikely to be published in the normal technical journals. Single copies are distributed free to interested individuals. Libraries, herpetological associations, and research laboratories are invited to exchange their publications with the Division of Amphibians and Reptiles. We wish to encourage individuals to share their bibliographies, translations, etc. with other herpetologists • through the SHIS series. If you have such items please contact George Zug for instructions on preparation and submission. Contributors receive 50 free copies. Please address all requests for copies and inquiries to George Zug, Division of Amphibians and Reptiles, National Museum of Natural History, Smithsonian Institution, Washington DC 20560 USA. Please include a self-addressed mailing label with requests. INTRODUCTION The herpetological collections of the Museo Nacional de Historia Natural (MNHNC) contains about 3500 amphibians and reptiles. Nearly 90% of the specimens are lizards, and of these, most are Liolaemus , the most diversified member of the Chilean herpetofauna. The specimens of Liolaemus derive mainly from "central Chile", i.e., the area between the city of La Serena and the Biobio River. Both northern and southern Chile are relatively unexplored; thus, the taxonomy and composition of these herpetof aunas is less well known. The distribution of Chilean lizards and snakes has not received much attention (however, see Valencia & Velosa 1981, Velosa & Navarro 1988) beyond the general information provided by Peters & Donoso-Barros (1970) and Donoso-Barros (1966, 1970). -
Chile & Easter Island 11
©Lonely Planet Publications Pty Ltd Chile & Easter Island Norte Grande p143 Easter Island Norte Chico (Rapa Nui) p190 p401 Santiago Middle Chile p44 p88 Sur Chico p220 Chiloé p277 Northern Patagonia p297 Southern Patagonia p338 Tierra del Fuego p379 Carolyn McCarthy, Cathy Brown, Mark Johanson, Kevin Raub, Regis St Louis PLAN YOUR TRIP ON THE ROAD Welcome to Chile . 6 SANTIAGO . 44 Cajón del Maipo . 83 Chile Map . .. 8 History . 45 Tres Valles . 86 Chile’s Top 20 . 10 Sights . 45 Activities . 61 MIDDLE CHILE . 88 Need to Know . 20 Courses . 62 Valparaíso & If You Like . 22 Tours . 63 the Central Coast . .. 89 Valparaíso . 89 Month by Month . 25 Festivals & Events . 64 Sleeping . .. 65 Viña Del Mar . 101 Itineraries . 28 Eating . 68 Casablanca Valley Wineries . 106 Chile Outdoors . 33 Drinking & Nightlife . 72 Quintay . 107 Travel with Children . 38 Entertainment . .74 Isla Negra . 108 Shopping . 75 Regions at a Glance . 40 Parque Nacional Around Santiago . 81 la Campana . 108 Maipo Valley Wineries . 81 Aconcagua Valley . 109 Pomaire . 82 Los Andes . 109 BAS VAN DEN HEUVEL/SHUTTERSTOCK © HEUVEL/SHUTTERSTOCK DEN VAN BAS © LARYLITVIN/SHUTTERSTOCK SANTIAGO’S BELLAVISTA PARQUE NACIONAL NEIGHBORHOOD P70 HUERQUEHUE P242 STEVE ALLEN/SHUTTERSTOCK © ALLEN/SHUTTERSTOCK STEVE © STEPHENS/SHUTTERSTOCK LUIS JOSE COLCHAGUA VALLEY P112 IGLESIA SAN FRANCISCO DE CASTRO P289 Contents Portillo . 110 Salto Del Laja . 134 Reserva Nacional Southern Heartland . 111 Los Angeles . 135 Los Flamencos . 158 Colchagua Valley . 112 Parque Nacional El Tatio Geysers . 160 Matanzas . 115 Laguna del Laja . 135 Calama . .. 161 Pichilemu . 115 Angol . 136 Chuquicamata . 163 Curicó . 118 Parque Nacional Antofagasta . .. 163 Nahuelbuta . 137 Parque Nacional South of Antofagasta . -
Caracterización Geoquímica Del Sistema Geotermal Termas De Puyehue-Aguas Calientes
Caracterización geoquímica del sistema geotermal Termas de Puyehue-Aguas Calientes Celis, R.1, 2, Reich, M. 1, 2 , Bascuñan, R. 3 (1) Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla Nº 803, Santiago, Chile . (2) Centro de Excelencia en Geotermia de los Andes (CEGA), Plaza Ercilla Nº 803, Santiago, Chile. (3) GTN-LA, AV. Parque Antonio Rabat Sur Nº 6165, Vitacura, Santiago, Chile. E-mail: [email protected] 1 Introducción los que pueden ser observados en algunos afloramientos con forma de brechas piroclásticas y tobas de lapilli o Un sistema geotermal posee tres características tefra. La presencia de tefras de lapilli es común en las principales: (i) una fuente de calor, (ii) un reservorio para laderas de conos piroclásticos jóvenes, mientras que las acumular calor, y (iii) una capa impermeable que rocas intrusivas que forman el basamento afloran sólo en mantenga el calor acumulado (Gupta & Roy, 2007). sitios puntuales. Estas son granodioritas/tonalitas y Existen diversos contextos geológicos donde estas granitos de dos edades distintas (Cretácico y Mioceno) características confluyen generando diferentes tipos de (Lara, en preparación). A lo largo de valles fluviales y en sistemas geotérmicos (Gupta & Roy, 2007). En Chile las partes bajas del área, los sedimentos Holocenos cubren existe una estrecha relación espacial entre las a las rocas ígneas, y como resultado de la glaciación y manifestaciones termales y los edificios volcánicos transporte fluvial, gruesas capas sedimentarias