The Volcanic Ash Soils of Chile

Total Page:16

File Type:pdf, Size:1020Kb

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. USE, MANAGEMENT AND PRODUCTIVITY OF THE MAIN KINDS OF ANDOSOLS IN CHILE 19 1. PRESENT PATTERNS OP SOIL USE 20 2. SOIL MANAGEMENT 22 (a) General management practices 22 (bj Tillage 24 (c; Soil moisture conservation, irrigation and drainage 25 id) Soil conservation 28 (e) Use of fertilizers 29 if) Crops and cropping systems 31 (g) Soil management problems 31 3. SOIL PRODUCTIVITY 33 4. ENGINEERING USES AND PROBLEMS 33 — iv — C. FARMING POTENTIALITIES OP A TRUMAO SPIL 34 1. A SUGGESTED FARM MANAGEMENT PROGRAM FOR MEDIT3M-SIZED PROPERTY ON SANTA BARBARA TRUMAO SOIL IN THE BIO-BIO, MALLECO OR NUBLE PROVINCES 35 Location and nature of farm in its original state 35 Modification of existing features 36 tö (i) Subdivision of fields 36 (ii) Pasture improvement 36 (iii) Internal aocess routes 36 (ivj Shelter belts 37 (v) Land cleaning and additional forest olearance 37 (vi) Reafforestation 37 (vii^ Drainage 37 (viii) Erosion oontrol 37 (ix^ Seleotion of farm machinery 38 (x) Farm buildings 38 (i±) Use and management of water 38 (xii) Management of pastures 38 (xiii ) Labour 38 (xiv) Control of weeds and pests 38 (c^ General plan of development 39 (d) Financing the development plan 41 (e) Technical assistance 41 D. NATURE. ORIGIN AND CLASSIFICATION OF CHILEAN ANDSOLS AND BELATED SOILS 42 1. TRUMAO SOILS OF ENVIRONMENTAL ZONE 1 (EXTREME NORTHERN TRUMAOS) 42 'a^ Environmental characteristics of the zone 42 bj General soil morphology 43 o) General chemical characteristics 43 d) Characteristics of typical soils 44 (i) Hornillos fine sandy loam 44 (ii) Maiten very fine sandy to silt loam 45 (iii) Tregualemu very fine sandy loam 46 (iv) Nirreguao fine sand 46 (v) Laguna del Maule loamy sand 47 Soil genesis 47 &j Soil classification 48 2. TRUMAO SOILS OF ENVIRONMENTAL ZONE 2 (NORTHERN TRUMAOS) 48 'a) Environmental characteristics of the zone 49 t) General soil morphology 50 c) General chemical characteristics 51 d) Characteristics of typical soils 52 (i) Santa Barbara very fine sandy loam, Chilian facies 53 (ii) Santa Barbara very fine sandy loam, Sta. Barbara facies 53 (iii) Santa Barbara very fine sandy loam, Mulchen facies 54 (iv) Arrayan silt loam 54 (v) Baguales fine sandy loam 55 Soil genesis 56 18 Soil classification 57 - V - Page 3. TRUMAO SOILS OF ENVIRONMENTAL ZONE 3 (CENTRAL TRUMAOS) 57 Environmental characteristics of the sons 58 General soil morphology 59 General chemical characteristics 60 Characteristics of typical soils 61 (i) Cantin silt loam 61 (ii) Icalma loamy coarse sand 62 (iii) Vilcün loam to silt loam 63 (iv) Temuco silt loam 64 (v) Trevolhue vexj fine sandy loam 64 Soil genesis 65 fe)Soi l classification 67 4. TRÜMAO SOILS OF ENVIRONMENTAL ZONE 4 (SOUTHERN TRUMAOS) 67 (a) Environmental characteristics of the zone 66 (b) General soil morphology 66 (c) General chemical characteristics 69 (d) Characteristics of typioal soils 69 (i) Puerto Octay silt loam and fine sandy loam 70 Puerto Fonok very fine sandy loam and silt loam 70 Puyehue silt loam 71 Choshuenco sandy loam 72 Rupanco gravelly coarse sandy loam 72 Quillelhue loamy sand 73 Puoón coarse sandy loam 73 Osorno yexj fine sandy loam 74 Pelch.uq.ufn fine sandy loam 74 Soil genesis 75 Soil classification 77 5. TRUMAO SOILS OF ENVIRONMENTAL ZONE 5 (EXTREME SOUTHERN TRUMAOS) 77 a) Environmental characteristics of the zone 73 h) General soil morphology 78 c) General ohemioal characteristics 79 d) Characteristics of typical soils 79 (i) Castro silt loam 80 (ii) Quellen silt loam 80 (iii) Maniuales silt loam 81 (iv) Puerto Lumaa sandy loam 81 (VJ Natri peaty fine sandy loam 82 (vi) Chepu very fine sandy loam 83 Soil genesis 84 felSoi l classification 85 6. TRUMAO SOILS OF ENVIRONMENTAL ZONE 6 (CHILEAN TROPICAL TRUMAOS) 85 (a) Environmental characteristics of the zone 85 (hJ General soil morphology 86 (o) General ohemioal oharaoteristiCB 86 (d) Charaoteristies of typioal soils 87 (i) Rano Kao heavy fine sandy loam 87 (ii j Vinapu very fine sandy loam 87 (iii) Poike silty clay loam 88 Soil genesis 88 Soil classification 89 - VI - 7. SADI SOILS 90 a) Environmental oharaoteristics of nadi soils 90 b) General morphology of nadi soils 90 c) General chemical characteristics 91 d) Characteristics of -typical nadi soils 91 (i) Pitrufquên heavy sandy loam 91 (ii) Frutillar silt loam 91 (iii) Carel fine sandy loam 92 (iv) Calonje very fine sandy loam 93 Soil genesis 93 fc)Soi l classification 94 8. TRÜMA0 SOILS ON STEEP SLOPES AND RELATED STEEPLAJSTD SOILS 95 (TRUMAO STEEPLAND SOILSJ a) Environmental characteristics of trumao steepland soils 95 b) General characteristics of trumao steepland soils 97 CJ General chemical characteristics 97 d) Characteristics of typioal soils 97 (i) Ataoaloo steepland soils 98 (iii Homolluco steepland soils 98 (iii) Chanleufu steepland soils 99 (iv) Peulla steepland soils 100 (v) Huemules steepland soils 101 Soil genesis 102 fe)Soi l classification 103 9. INTERGRADES BETWEEHT TRUMAO SOILS AND OTHER SOIL GROUPS 104 (a) Intergrades to recent volcanic ash soils 104 1. General features 104 2. Typical intergrades 104 (i} Chilian sandy intergrading to Santa Barbara sandy loam 104 (ii) Lonquimay 00arse sand and gravel 105 (iii) Tillarrica coarse sand 105 (iv) Antillanca stony sand 1°5 (b) Intergrades to red voloanio days 106 (i) Collipulli sandy loam 106 (ii) Maquehue loam 107 10. INTERGRADES HETWEEN HADI SOILS ABD OTHER SOIL GROUPS 107 (a) Intergrades to Humic Gley soils 107 - General features 107 (i) Freire silty day loam 107 (b) Intergrades to Podzolic Gleys and Oley Podzols 107 - General features 107 (i) Maldonado peaty sandy loam 108 BIBLIOGRAPHT 1°9 APPENDIX It PROFILE DESCRIPTIONS OP SOILS MEHTIOHED IH THE TEXT' 117 APPEHDIX lit THE RED VOLCAHIC CLAYS OF CHILE 179 EXPLANATORY LEGENDS FOR FIGS. 4 AND 10 193 - vii- LIST OF glOURES Figure 1 - Voloanio Regions Bordering the Paoific Ocean Figure 2 - Distribution of Voloanio Ash Material in Chile Figure 3 - Distribution of Andosols and "Red Voloanic Clays" Figure 4 - Broad Distribution of Volcanic Ash Soils in Southern Chile Figure 5 — Approximate Mean Annual Rainfall Figure 6 - Approximate number of months with less than 100 m.m. rainfall Figure 7 - Approximate Mean Annual Temperatures Figure 8 - Broad Topographio Units Figure 9 - Broad Distribution of Primitive Plant Cover Figure 10 - Environmental Regions of the Southern Andean Zone Figure 11.A - Transeot, South-Central Chile in Latitude 40° 38'S Figure 11.B - Diagrammatio Section Across Nadi Terraces Showing Relative Depth of the Ash Mantle MR/26617 INTRODUCTION In accordance with the Agreement signed between the Government of Chile and the Food & Agriculture Organization of the united Nations (FAO), a specialist in voloanic ash soils, Mr A.C.S.Wright, was made available by FAO to study the nature and agricultural potential of the volcanic ash soils of Chile. Mr Wright was in Chile from December 1959 to March 1964« His terms of reference were to advise and assist the Government — 1. In the study of the morphology, genesis and classification of the soils derived from volcanic ash. 2. In establishing correlations between volcanic soils in Chile and similar soils occurring in New Zealand. 3. In determining, for each of the major volcanic soils, its suitability for crops, pasture or forestry production, considering problems of management, irrigation, drainage, fixation of phosphate, etc. ACKNOWLEDGEMENTS The expert wishes to express his appreciation to the offioials of the Government of Chile, especially to the late Dr. Carlos Diaz Vial and Sr. Mario Feralta Peralta of the Ministry of Agriculture, and to Sr. Elias Letelier, for their unfailing support and constant readiness to provide advice and assistance during the progress of the work. In carrying out the work, the expert spent a large amount of time in the field with the various members of the soil survey team of the Ministry of Agriculture. These were most fruitful days, and the expert wishes to express his thanks to all these Ingeneiros Agronomos for their ready acceptance of the 'gringo from New Zealand', for their keen collaboration, great hospitality and sincere friendship.
Recommended publications
  • 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.
    [Show full text]
  • Universita' Degli Studi Di Milano Bicocca
    Dipartimento di Scienze Ambiente e Territorio e Scienze della Terra Università degli studi di Milano-Bicocca Dottorato di Ricerca in Scienze della Terra XXVI ciclo Earthquake-induced static stress change in promoting eruptions Tutore: Prof. Alessandro TIBALDI Co-tutore: Dott.ssa Claudia CORAZZATO Fabio Luca BONALI Matr. Nr. 040546 This work is dedicated to my uncle Eugenio Marcora who led my interest in Earth Sciences and Astronomy during my childhood Abstract The aim of this PhD work is to study how earthquakes could favour new eruptions, focusing the attention on earthquake-induced static effects in three different case sites. As a first case site, I studied how earthquake-induced crustal dilatation could trigger new eruptions at mud volcanoes in Azerbaijan. Particular attention was then devoted to contribute to the understanding of how earthquake-induced magma pathway unclamping could favour new volcanic activity along the Alaska-Aleutian and Chilean volcanic arcs, where 9 seismic events with Mw ≥ 8 occurred in the last century. Regarding mud volcanoes, I studied the effects of two earthquakes of Mw 6.18 and 6.08 occurred in the Caspian Sea on November 25, 2000 close to Baku city, Azerbaijan. A total of 33 eruptions occurred at 24 mud volcanoes within a maximum distance of 108 km from the epicentres in the five years following the earthquakes. Results show that crustal dilatation might have triggered only 7 eruptions at a maximum distance of about 60 km from the epicentres and within 3 years. Dynamic rather than static strain is thus likely to have been the dominating “promoting” factor because it affected all the studied unrested volcanoes and its magnitude was much larger.
    [Show full text]
  • Global Transmission Weekly Update on the Global Electricity Transmission Industry
    September 03, 2012 Global Transmission Weekly Update on the global electricity transmission industry INSIDE THIS ISSUE NORTH AMERICA 2 PJM cancels PATH and MAPP projects 2 Rock Island Clean Line project faces opposition in Illinois 2 Opposition against Champlain-Hudson Power Express transmission line growing 2 Clean Line hosts public meetings for Grain Belt Express line 3 Entergy Arkansas files testimony with state PSC 3 Entergy proposal of shifting ICT services to MISO attracts strong opposition 3 MISO approves scaled down version of Bay Lake Project 3 Enbridge repays USD151 million federal loan 4 I-5 Corridor to cost USD12 million to tax payers 4 NWE and BPA announce transmission upgrades in Montana 4 CWL proposes third route option for Mill Creek substation transmission lines 4 TVA hosts public meeting for 161 kV line in Mississippi 5 MEC selects route for 69 kV transmission line 5 PPM files request with Texas PUC against high congestion cost 5 SDG&E’s ECO project receives approval from DoI 5 PAR Electrical bags high voltage contracts from SCE 5 ABB receives USD60 million HVDC contract from AEP 6 LATIN AMERICA 6 Brazilian bank extends BRL1 billion loan for HPP lines 6 Brazilian power utility to spend BRL700 million to link wind projects 6 Argentinean regulator to hold hearing for 500 kV Santa Fe project 7 Chilean power company submits environmental request for 220 kV project 7 Chilean solar company submits environmental declaration for 110 kV line 7 Mexican energy regulator formulates smart grid plan 7 Venezuelan power utility to auction
    [Show full text]
  • Downloaded 09/26/21 05:17 AM UTC 1930 JOURNAL of HYDROMETEOROLOGY VOLUME 18
    JULY 2017 G O N Z Á LEZ-REYES ET AL. 1929 Spatiotemporal Variations in Hydroclimate across the Mediterranean Andes (30°–37°S) since the Early Twentieth Century a b c ÁLVARO GONZÁLEZ-REYES, JAMES MCPHEE, DUNCAN A. CHRISTIE, d e f f CARLOS LE QUESNE, PAUL SZEJNER, MARIANO H. MASIOKAS, RICARDO VILLALBA, g f ARIEL A. MUÑOZ, AND SEBASTIÁN CRESPO a Instituto de Ciencias de la Tierra, Facultad de Ciencias, Universidad Austral de Chile, Valdivia, Chile b Departamento de Ingenierı´a Civil and Advanced Mining Technology Center, Facultad de Ciencias Fı´sicas y Matemáticas, Universidad de Chile, Santiago, Chile c Laboratorio de Dendrocronologı´a y Cambio Global, Instituto de Conservación Biodiversidad y Territorio, Facultad de Ciencias Forestales y Recursos Naturales, Universidad Austral de Chile, Valdivia, and Center for Climate and Resilience Research (CR)2, Universidad de Chile, Santiago, Chile d Laboratorio de Dendrocronologı´a y Cambio Global, Instituto de Conservación Biodiversidad y Territorio, Facultad de Ciencias Forestales y Recursos Naturales, Universidad Austral de Chile, Valdivia, Chile e Laboratory of Tree-Ring Research, and School of Natural Resources and the Environment, The University of Arizona, Tucson, Arizona f Instituto Argentino de Nivologı´a, Glaciologı´a y Ciencias Ambientales, CCT CONICET Mendoza, Mendoza, Argentina g Instituto de Geografı´a, Pontificia Universidad Católica de Valparaı´so, Valparaı´so, Chile (Manuscript received 13 January 2016, in final form 10 January 2017) ABSTRACT In the Mediterranean Andes region (MA; 308–378S), the main rivers are largely fed by melting snowpack and provide freshwater to around 10 million people on both sides of the Andes Mountains.
    [Show full text]
  • Rapid Magma Ascent and Generation of Th Excesses in the Lower Crust At
    Earth and Planetary Science Letters 255 (2007) 229–242 www.elsevier.com/locate/epsl Rapid magma ascent and generation of 230Th excesses in the lower crust at Puyehue–Cordón Caulle, Southern Volcanic Zone, Chile ⁎ Brian R. Jicha a, , Brad S. Singer a, Brian L. Beard a, Clark M. Johnson a, Hugo Moreno-Roa b,c, José Antonio Naranjo b a Department of Geology and Geophysics, University of Wisconsin—Madison, 1215 West Dayton Street, Madison WI 53706, USA b Servicio Nacional de Geología y Minería (SERNAGEOMIN), Avenida Santa María, 0104 Santiago, Chile c Observatorio Volcanologico de los Andes del Sur (OVDAS), Cerro Ñielol-Sector Antenas, Temuco, Chile Received 28 July 2006; received in revised form 7 December 2006; accepted 8 December 2006 Available online 30 January 2007 Editor: R.W. Carlson Abstract Basaltic to rhyolitic lavas and tephras erupted over the last 70 kyr at the Puyehue–Cordón Caulle volcanic complex in the Andean Southern Volcanic Zone (SVZ) were analyzed for major and trace element, Sr isotope, and U–Th isotope compositions to constrain the timescales of magmatic processes and identify the subducted and crustal components involved in magma genesis. Internal U–Th mineral isochrons from five lavas and three tephra fall deposits are indistinguishable from their eruption ages, indicating a short period (b1000 yr) of crystal residence in the magma prior to eruption. The (230Th/232Th) ratios define a narrow range (0.80–0.83) compared to that of all SVZ lavas (0.72–0.97), suggesting that Puyehue basalt was derived from a relatively uniform mantle source. Dacites and rhyolites have the largest U excesses and likely evolved via fractional crystallization of a plagioclase-dominated mineral assemblage.
    [Show full text]
  • Pudu in a Chilean National Park
    547 Pudu in a Chilean National Park Gary 8. Wetterberg The Chilean pudu Pudu pudu, the smallest American deer, is on the world list of endangered species in the IUCN Red Data Book. One of its few remaining refuges is in the Vicente Perez Rosales National Park. This is in the Lake District of southern Chile, the 'Switzerland of South America', between the Puyehue National Park to the north, and the Nahuel Huapi National Park in Argentina on the east. There are very few records on the fauna of this park, which covers 243,000 hectares, and is part of the Patagonian Subdivision of the Neotropical Faunal Region. Like an Island In many ways, Chile is like an island, cut off by the Atacama Desert on the north, the Andes to the east, the Patagonian ice fields and fiords to the south, and the Pacific on the west. This geo- graphical isolation has permitted the development of a unique biota, and Chilean wildlife exhibits some of the characteristics of island fauna such as narrow endemics and few competitors. The pudu is descended from the deer that migrated from North America in the late Tertiary period (Simpson 1950). The species is primarily of Chilean origin and distribution, although it is frequently encountered in adjacent areas of Argentina, and is present in Bolivia (Walker, 1964). It was discovered and named in 1782 by the Jesuit Juan Ignacio Molina, the 'father of Chilean natural history' (Osgood, 1943). Other species of the genus are found in Ecuador and Peru (Grimwood, 1968), and Brazil (Hershkovitz, 1958).
    [Show full text]
  • Global Prospects for Dairy in Argentina and Chile: Evidence from Field Visits and Model Simulations
    Global Prospects for Dairy in Argentina and Chile: Evidence from Field Visits and Model Simulations Frank H. Fuller, John C. Beghin, Michael Boland, Bruce A. Babcock, and William Foster MATRIC Briefing Paper 06-MBP 11 August 2006 Midwest Agribusiness Trade and Research Information Center Iowa State University Ames, Iowa 50011-1070 www.matric.iastate.edu Frank Fuller is a research scientist with the Center for Agricultural and Rural Development at Iowa State University; John Beghin is professor and Martin Cole Chair in International Agricultural Economics at Iowa State University; Bruce Babcock is director of the Center for Agricultural and Rural Development and professor of economics at Iowa State University; Michael Boland is a professor of agricultural economics, and associate director of the Arthur Capper Cooperative Center at Kansas State University; and William Foster is professor of agricultural economics at Pontificia Universidad Católica de Chile in Santiago. This paper is available online on the CARD Web site: www.card.iastate.edu. Permission is granted to reproduce this information with appropriate attribution to the authors. For questions or comments about the contents of this paper, please contact Frank Fuller, 575 Heady Hall, Iowa State University, Ames, IA 50011-1070; Ph: 515-294-2364; Fax: 515-294-6336; E-mail: [email protected]. MATRIC is supported by the Cooperative State Research, Education, and Extension Service, U.S. Department of Agriculture, under Agreement No. 92-34285-7175. Any opinions, findings, conclusions, or recommendations expressed in this publication are those of the authors and do not necessarily reflect the view of the U.S. Department of Agriculture.
    [Show full text]
  • Fish Surface Activity and Pursuit-Plunging by Olivaceous Cormorants
    SHORT COMMUNICATIONS 327 At the Missouri site, eagles had access to large numbers of crippled and dead geese, which presumably were the primary source oflead shot. In South Dakota, Steenhof(1976) reported finding waterfowl remains in 285 of 363 egested pellets including 10 (2.7%) with lead shot. Based upon her observations, she concluded eagles obtained most of the waterfowl in upland fields. Likewise, at our Nebraska site, eagles ate waterfowl that had been feeding in upland fields (obtained by kleptoparasitizing other raptors [Jorde and Lingle, in press]). In March 1980, they also scavenged waterfowl that had died of avian cholera (Lingle and Krapu 1986). Infrequent ingestion of lead shot by Bald Eagles in Nebraska probably stems from a low incidence of lead shot among waterfowl wintering along the Platte and North Platte rivers. The frequency of occurrence of lead shot in wintering waterfowl in Nebraska is not known; however, only about 1% of waterfowl wintering in the Texas High Plains region during the same period had lead shot in their digestive tracts (Wallace et al. 1983). It is probable that field-feeding Mallards obtained in lightly hunted uplands contain fewer lead shot than cripples or segments of the population feeding principally in wetlands where hunting activity and lead shot contamination arc likely to be concentrated. Acknowledgments.-We thank the following field technicians: R. Atkins, J. Cochnar, M. Hay, C. House, D. Janke, D. Jenson, and W. Norling. T. Baskett, D. Johnson, D. Jorde, and P. Pietz critically reviewed the manuscript. LITERATURE CITED GRIFFIN,C. R., T. S. BASKETT,AND R.
    [Show full text]
  • Chile: a Journey to the End of the World in Search of Temperate Rainforest Giants
    Eliot Barden Kew Diploma Course 53 July 2017 Chile: A Journey to the end of the world in search of Temperate Rainforest Giants Valdivian Rainforest at Alerce Andino Author May 2017 1 Eliot Barden Kew Diploma Course 53 July 2017 Table of Contents 1. Title Page 2. Contents 3. Table of Figures/Introduction 4. Introduction Continued 5. Introduction Continued 6. Aims 7. Aims Continued / Itinerary 8. Itinerary Continued / Objective / the Santiago Metropolitan Park 9. The Santiago Metropolitan Park Continued 10. The Santiago Metropolitan Park Continued 11. Jardín Botánico Chagual / Jardin Botanico Nacional, Viña del Mar 12. Jardin Botanico Nacional Viña del Mar Continued 13. Jardin Botanico Nacional Viña del Mar Continued 14. Jardin Botanico Nacional Viña del Mar Continued / La Campana National Park 15. La Campana National Park Continued / Huilo Huilo Biological Reserve Valdivian Temperate Rainforest 16. Huilo Huilo Biological Reserve Valdivian Temperate Rainforest Continued 17. Huilo Huilo Biological Reserve Valdivian Temperate Rainforest Continued 18. Huilo Huilo Biological Reserve Valdivian Temperate Rainforest Continued / Volcano Osorno 19. Volcano Osorno Continued / Vicente Perez Rosales National Park 20. Vicente Perez Rosales National Park Continued / Alerce Andino National Park 21. Alerce Andino National Park Continued 22. Francisco Coloane Marine Park 23. Francisco Coloane Marine Park Continued 24. Francisco Coloane Marine Park Continued / Outcomes 25. Expenditure / Thank you 2 Eliot Barden Kew Diploma Course 53 July 2017 Table of Figures Figure 1.) Valdivian Temperate Rainforest Alerce Andino [Photograph; Author] May (2017) Figure 2. Map of National parks of Chile Figure 3. Map of Chile Figure 4. Santiago Metropolitan Park [Photograph; Author] May (2017) Figure 5.
    [Show full text]
  • 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.
    [Show full text]
  • Scorpiones; Bothriuridae) with the First Record from Argentina
    Rev. Mus. Argentino Cienc. Nat., n.s. 15(1): 113-120, 2013 ISSN 1514-5158 (impresa) ISSN 1853-0400 (en línea) New distributional data on the genus Phoniocercus Pocock, 1893 (Scorpiones; Bothriuridae) with the first record from Argentina Andrés A. OJANGUREN-AFFILASTRO 1, Jaime PIZARRO-ARAYA 2 & Richard D. SAGE 3 1 Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, División Aracnología, Av. Ángel Gallardo 470, 1405DJR Buenos Aires, Argentina. [email protected] 2 Laboratorio de Entomología Ecológica, Departamento de Biología, Facultad de Ciencias, Universidad de La Serena, Casilla 599, La Serena, Chile. [email protected] 3 Sociedad Naturalista Andino Patagónica (SNAP), Paso Juramento 190, 3° piso, 8400 Bariloche, Río Negro, Argentina. [email protected] Abstract: Scorpion genus Phoniocercus Pocock, 1893 (Bothriuridae) is endemic to the cold humid forests of the southwestern part of South America. Up to now the known distribution of the genus was restricted to the Valdivian forests of southern Chile. In this contribution we present the first record from Argentina and the first records from central Chile. New data about their ecology and systematics are also presented. Key words: Scorpiones, Phoniocercus, distribution, Chile, Argentina, new records. Resumen: Nuevos datos de distribución del género Phoniocercus Pocock, 1893 (Scorpiones; Bothriurdae) con el primer registro para Argentina. El género de escorpiones Phoniocercus Pocock, 1893 (Bothriuridae) es endémico de los bosques húmedos y fríos del sudoeste de América del Sur. Hasta ahora la dis- tribución conocida del mismo se encontraba restringida a los bosques Valdivianos del sur de Chile. En esta con- tribución presentamos el primer registro de la Argentina y los primeros registros del centro de Chile.
    [Show full text]
  • Depth of Differentiation Under Osorno Volcano (Chile)
    Depth of differentiation under Osorno volcano (Chile) T.Bechona, J. Vander Auweraa, O. Namurb, P. Fugmanna, O. Bollea, L. Larac aUniversity of Liège – Department of Geology bUniversity of Leuven – Department of Earth and Environmental Sciences cSERNAGEOMIN Introduction What is the depth of the magma chamber at Osorno volcanoCredit ? : H. Foucart It matters for : • Understanding differentiation in young arcs. Estimations evidence the major role of arc magmatism in the construction of continental crust (up to 60% : Rudnick and Gao, 2003). • Monitoring a major flank collapse like the one of Mt St Helens in 1980s (USA) 2 Introduction ↑ Ryan et al. (2009) Modified Credit : H. Foucart 3 ↑ After Stern et al 2007, modified by P. Fugmann Method T°C and P (kbar) of last Lee et al 2009 equilibration with mantle Assuming H2O (1%) Assuming P (0-5kbar) and H2O (0-5%) • Whole rock major elements: XRF Putirka 2008 T°C: Wan et al 2007 • Minerals major Coogan et al 2014 elements: microprobe Harrisson et Watson 1984 Depth P (kbar): Putirka 2008 Tassara et Echaurren Neave et Putirka 2017 (km): 2012 Assuming H2O 4 Results Trachy- Trachyte Basaltic- Andesite Trachy- Andesite Trachy- Basalts Basaltic- Basalts Andesites Dacites Andesites 5 Results Trachy- Trachyte Basaltic- Andesite Trachy- Andesite In addition : • Magma compositions results from fractional crystallization (mass balance model +traceTrachy elements- diagrams) Basalts • Dominant mineral phases : Ol + Plag in mafic rocks • Rather low water content (No hydrated phases except in one dacite) Basaltic- Basalts Andesites Dacites Andesites 6 Results ↑ Putirka (2008) 7 Results T°C and P° 8 Discussion P° (kbar) H2O (%wt) 9 ↓ Seismic data from SERNAGEOMIN surveillance (Chile) Discussion W E Sea level 1 Kbar 2 Kbar 3 Kbar 10 Discussion 1-3 Kbar Using crustal model of Tassara and Magma chamber Echaurren (2012) ←↓ P° ~ 11-12 Kbar Last peridotite equilibrium T°C~ 1335°C 11 Discussion N S Crustal 2 disc.
    [Show full text]