Chile Relish Sleds Down the Fixed Ropes from High Camp to Low Camp
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Report on Cartography in the Republic of Chile 2011 - 2015
REPORT ON CARTOGRAPHY IN CHILE: 2011 - 2015 ARMY OF CHILE MILITARY GEOGRAPHIC INSTITUTE OF CHILE REPORT ON CARTOGRAPHY IN THE REPUBLIC OF CHILE 2011 - 2015 PRESENTED BY THE CHILEAN NATIONAL COMMITTEE OF THE INTERNATIONAL CARTOGRAPHIC ASSOCIATION AT THE SIXTEENTH GENERAL ASSEMBLY OF THE INTERNATIONAL CARTOGRAPHIC ASSOCIATION AUGUST 2015 1 REPORT ON CARTOGRAPHY IN CHILE: 2011 - 2015 CONTENTS Page Contents 2 1: CHILEAN NATIONAL COMMITTEE OF THE ICA 3 1.1. Introduction 3 1.2. Chilean ICA National Committee during 2011 - 2015 5 1.3. Chile and the International Cartographic Conferences of the ICA 6 2: MULTI-INSTITUTIONAL ACTIVITIES 6 2.1 National Spatial Data Infrastructure of Chile 6 2.2. Pan-American Institute for Geography and History – PAIGH 8 2.3. SSOT: Chilean Satellite 9 3: STATE AND PUBLIC INSTITUTIONS 10 3.1. Military Geographic Institute - IGM 10 3.2. Hydrographic and Oceanographic Service of the Chilean Navy – SHOA 12 3.3. Aero-Photogrammetric Service of the Air Force – SAF 14 3.4. Agriculture Ministry and Dependent Agencies 15 3.5. National Geological and Mining Service – SERNAGEOMIN 18 3.6. Other Government Ministries and Specialized Agencies 19 3.7. Regional and Local Government Bodies 21 4: ACADEMIC, EDUCATIONAL AND TRAINING SECTOR 21 4.1 Metropolitan Technological University – UTEM 21 4.2 Universities with Geosciences Courses 23 4.3 Military Polytechnic Academy 25 5: THE PRIVATE SECTOR 26 6: ACKNOWLEDGEMENTS AND ACRONYMS 28 ANNEX 1. List of SERNAGEOMIN Maps 29 ANNEX 2. Report from CENGEO (University of Talca) 37 2 REPORT ON CARTOGRAPHY IN CHILE: 2011 - 2015 PART ONE: CHILEAN NATIONAL COMMITTEE OF THE ICA 1.1: Introduction 1.1.1. -
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. -
Volcán Tupungatito
Volcán Tupungatito Región: Metropolitana Provincia: Cordillera Comuna: San José de Maipo Coordenadas: 33°23’S – 69°50’O Poblados más cercanos: El Alfalfal – los Maitenes – El Manzano Tipo de volcán: Estratovolcán Altura: 5603 m s.n.m. Diámetro basal: 7,5 km Área basal: 44 km2 Volumen estimado: 30 km3 Volcán Tupungatito. Vista desde el noroeste Última actividad: 1986 (Fotografía: Carolina Silva, SERNAGEOMIN) Última erupción mayor: 1959-1960 Ranking de riesgo 22 específico: Generalidades El volcán Tupungatito corresponde a un estratovolcán de corta vida (< 80 ka) y reducido volumen. Está emplazado en el extremo septentrional de la Zona Volcánica Sur de los Andes, a 75 km al este de Santiago. Forma parte de un grupo volcánico donde destacan los volcanes Tupungato y Nevado Sin Nombre, ambos inactivos. Durante su fase inicial este volcán registró una importante actividad efusiva, con generación de coladas de lava de hasta 18 km de alcance encauzadas en torno al valle del río Colorado, además de lahares, flujos piroclásticos y avalanchas de detritos de mediano alcance. Durante el Holoceno su actividad cambió a un estilo mixto (efusivo/explosivo), donde además de las coladas de lava se tiene registro de erupciones mayoritariamente vulcanianas. Este aumento en la actividad explosiva ha construido un sistema cratérico hacia la cumbre del volcán, el cual se localiza cercano a una depresión semi-circular de 4 km de diámetro rellena por un glaciar. En la actualidad exhibe actividad fumarólica intensa y permanente concentrada en uno de estos cráteres el cual, además, hospeda un lago ácido. Registro eruptivo Los registros de erupciones mencionan una veintena de eventos desde el siglo XVII, los que incluyen reactivaciones menores e incrementos en la actividad fumarólica. -
Manual-Procedimiento Caída Cenizas Volcánicas
MANUAL DE PROCEDIMIENTOS ANTE CAIDA DE CENIZAS VOLCANICAS Grupo de Estudio y Seguimiento de Volcanes Activos Proyecto “Exactas con la Sociedad” Facultad de Ciencias Exactas y Naturales – Universidad de Buenos Aires -2010- Autores Dr. Alberto Tomás Caselli Lic. María Laura Vélez Lic. Mariano Roberto Agusto Lic. María Laila Jover Colaboradores especiales Dra. Leonor Bonan Lic. Cintia Lorena Bengoa Srta. Diana Luz Sierra Lic. Ana María Fazio Prof. Patricia Castaño Dra. Ana Monasterio (EPROTEN) Ing. Agr. Carlos Prior (SENASA Zapala) Dr. Manuel Rivera (Coordinador de Emergencias Sanitarias Neuquén) Ing. Agr. Raúl Coppa (INTA Esquel) AGRADECIMIENTOS Los autores desean expresar su agradecimiento a todas las personas que brindaron información durante la recopilación realizada en las localidades en las que se hicieron entrevistas. En especial, queremos destacar la colaboración de los Intendentes de las municipalidades de Esquel, Trevelin, Corcovado, Los Antiguos y Caviahue-Copahue por la gran predisposición para responder nuestras consultas y contactarnos con el personal que actuó en la emergencia. En particular agradecemos al Intendente de la Municipalidad de Esquel Rafael Williams, al Secretario Gobierno Gustavo Lucero y colaboradores como Karina Araqué y Pablo Schulz, quienes se reunieron especialmente con nosotros y nos brindaron toda la información sobre la experiencia vivida. En la localidad de Trevelin, deseamos agradecer a Susana Thomas (Secretaria de Coordinación de Gabinete Municipalidad de Trevelin) y Alejandro Sabelli por la gran colaboración ofrecida y realizar los cuestionarios en la escuela publica, material de gran utilidad para acercarnos a la problemática de la población. Por otro lado, también agradecer al Intendente de la localidad de Corcovado, Héctor Diez y colaboradores, por la útil información brindada, en especial a lo referido a la región rural. -
Late Pleistocene and Holocene Tephrochronology of Mendoza Province, Argentina
O EOL GIC G A D D A E D C E I H C I L E O S F u n 2 d 6 la serena octubre 2015 ada en 19 Late Pleistocene and Holocene tephrochronology of Mendoza Province, Argentina Andres Bosch1; Charles R Stern*1 and Stella M. Moreiras2 1Department of Geological Sciences, University of Colorado, CB-399, Boulder, Colorado 80309-0399 USA 2CONICET,)Instituto)Argentino)de)Nivología,)Glaciología)y)Ciencias)Ambientales,)Mendoza,)CP5500,)Argentina Email: [email protected]! Abstract. Rhyolitic pyroclastic flows and tephra from the al., 1984) and Calabozos (300 and 150 ka; Hildreth et al., Pleistocene (450 ± 60 ka) eruption of the Laguna Diamante 1984) calderas have also been well documented. Here we caldera comprise the largest volume of pyroclastic material present preliminary results from a study in progress of late in northwest Mendoza Province. However, trace-element Pleistocene and Holocene tephra deposits in the province data indicate that 1-3 meter thick rhyolite tephra deposits, of Mendoza, Argentina. These results indicate that large which outcrop on both the southwest (Cacheuta) and late Pleistocene tephra deposits around the city of northeast (Borbollon) margins of the city of Mendoza, have Mendoza were not derived from the 450 ka Laguna an independent origin. These chemical data, and Diamante eruption, but from multiple younger eruptions of preliminary chronology, imply at least two different large some other source, and that numerous Holocene tephra late Pleistocene eruptions, both younger than that of the Diamante caldera, possibly of Tupungato volcano or the deposits outcropping along the Andean precordillera Tupungatito caldera. -
Glacier Albedo Reduction and Drought Effects in the Extratropical Andes, 1986–2020
Journal of Glaciology Glacier albedo reduction and drought effects in the extratropical Andes, 1986–2020 Thomas E. Shaw1,2 , Genesis Ulloa3, David Farías-Barahona4, 3 3,5 2,6 Article Rodrigo Fernandez , Jose M. Lattus and James McPhee 1 2 Cite this article: Shaw TE, Ulloa G, Farías- Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf, Switzerland; Advanced Barahona D, Fernandez R, Lattus JM, McPhee J Mining Technology Center, Universidad de Chile, Santiago, Chile; 3Department of Geology, Universidad de Chile, (2021). Glacier albedo reduction and drought Santiago, Chile; 4Institute für Geographie, Friedrich-Alexander-Universität Erlangen-Nürnberg, Erlangen, Germany; effects in the extratropical Andes, 1986–2020. 5SRGIS: Geología y Geomática Ltda, Santiago, Chile and 6Department of Civil Engineering, Universidad de Chile, – Journal of Glaciology 67(261), 158 169. https:// Santiago, Chile doi.org/10.1017/jog.2020.102 Received: 10 August 2020 Abstract Revised: 10 November 2020 Surface albedo typically dominates the mass balance of mountain glaciers, though long-term Accepted: 11 November 2020 First published online: 17 December 2020 trends and patterns of glacier albedo are seldom explored. We calculated broadband shortwave albedo for glaciers in the central Chilean Andes (33–34°S) using end-of-summer Landsat scenes Key words: between 1986 and 2020. We found a high inter-annual variability of glacier-wide albedo that is Albedo; Andes; climate; drought; glacier; largely a function of the glacier fractional snow-covered area and the total precipitation of the remote sensing preceding hydrological year (up to 69% of the inter-annual variance explained). Under the Author for correspondence: 2010–2020 ‘Mega Drought’ period, the mean albedo, regionally averaged ranging from ∼0.25– Thomas E. -
USGS Open-File Report 2009-1133, V. 1.2, Table 3
Table 3. (following pages). Spreadsheet of volcanoes of the world with eruption type assignments for each volcano. [Columns are as follows: A, Catalog of Active Volcanoes of the World (CAVW) volcano identification number; E, volcano name; F, country in which the volcano resides; H, volcano latitude; I, position north or south of the equator (N, north, S, south); K, volcano longitude; L, position east or west of the Greenwich Meridian (E, east, W, west); M, volcano elevation in meters above mean sea level; N, volcano type as defined in the Smithsonian database (Siebert and Simkin, 2002-9); P, eruption type for eruption source parameter assignment, as described in this document. An Excel spreadsheet of this table accompanies this document.] Volcanoes of the World with ESP, v 1.2.xls AE FHIKLMNP 1 NUMBER NAME LOCATION LATITUDE NS LONGITUDE EW ELEV TYPE ERUPTION TYPE 2 0100-01- West Eifel Volc Field Germany 50.17 N 6.85 E 600 Maars S0 3 0100-02- Chaîne des Puys France 45.775 N 2.97 E 1464 Cinder cones M0 4 0100-03- Olot Volc Field Spain 42.17 N 2.53 E 893 Pyroclastic cones M0 5 0100-04- Calatrava Volc Field Spain 38.87 N 4.02 W 1117 Pyroclastic cones M0 6 0101-001 Larderello Italy 43.25 N 10.87 E 500 Explosion craters S0 7 0101-003 Vulsini Italy 42.60 N 11.93 E 800 Caldera S0 8 0101-004 Alban Hills Italy 41.73 N 12.70 E 949 Caldera S0 9 0101-01= Campi Flegrei Italy 40.827 N 14.139 E 458 Caldera S0 10 0101-02= Vesuvius Italy 40.821 N 14.426 E 1281 Somma volcano S2 11 0101-03= Ischia Italy 40.73 N 13.897 E 789 Complex volcano S0 12 0101-041 -
Supplementary Material
Supplementary Material In the following, the relevant data sets and test results, together with the corresponding figures, are shown for each volcano, together with a short comment on the volcano characteristics and the fit quality. The names adopted for the repose time fit parameters are exponential distribution: Weibull distribution: log-logistic distribution: Tupungatito year VEI year VEI year VEI Tupungatito Volcano is located in the high Andes east of Chile's capital 1829 2 1925 2 1961 2 Santiago, which is inhabited by six million people and by far Chile's 1835 2? 1946 2 1964 2 most important industrial and commercial centre. The volcano built up 1861 2 1958 2 1968 2 since Pleistocene times in the Nevado Sin Nombre Caldera (Siebert and 1889 2 1959 2 1980 2 Simkin, 2002), its recent activity consists of 18 smaller historical 1897 2 1959 2 1986 1 eruptions, which produced a total erupted volume of about 6 km³ 1901 2 1960 2 1987 2 (Sruoga et al., 1993). 1907 2 2 fit A t k d x0 p ²/DoF R KS-diff. AICc exp. 15.17±0.36 10.57±0.39 0.384 0.978 0.097 14.0 16± 0 9.97±0.27 0.442 0.974 0.095 14.0 WB 15.37±0.98 0.0970 0.9297 0.364 0.975 0.108 15.1 ±0.009 ±0.092 16± 0 0.1023 0.8811 0.356 0.975 0.126 13.3 ±0.003 ±0.039 log 15.04±0.51 6.881 1.494 0.445 0.976 0.134 17.1 ±0.470 ±0.097 16± 0 6.140 1.385 0.479 0.973 0.177 16.5 ±0.247 ±0.072 KS-threshold: 0.328 all fits pass the K-S-test The difference in AICc for fixed vs. -
Across-Arc Geochemical Variations in the Southern Volcanic Zone, Chile (34.5–38.0°S): Constraints on Mantle Wedge and Slab Input Compositions
Available online at www.sciencedirect.com Geochimica et Cosmochimica Acta 123 (2013) 218–243 www.elsevier.com/locate/gca Across-arc geochemical variations in the Southern Volcanic Zone, Chile (34.5–38.0°S): Constraints on mantle wedge and slab input compositions G. Jacques a,⇑, K. Hoernle a,b, J. Gill c, F. Hauff b, H. Wehrmann a, D. Garbe-Scho¨nberg d, P. van den Bogaard a,b, I. Bindeman e, L.E. Lara f a Collaborative Research Center (SFB574), University of Kiel and GEOMAR, 24148 Kiel, Germany b GEOMAR Helmholtz Centre for Ocean Research Kiel, 24148 Kiel, Germany c University of California, Santa Cruz, CA 95064, USA d Institute of Geosciences of the University of Kiel, 24118 Kiel, Germany e University of Oregon, Eugene, OR 97403, USA f Servicio Nacional de Geologı´a y Minerı´a, Santiago, Chile Received 7 September 2012; accepted in revised form 13 May 2013; available online 23 May 2013 Abstract Crustal assimilation (e.g. Hildreth and Moorbath, 1988) and/or subduction erosion (e.g. Stern, 1991; Kay et al., 2005) are believed to control the geochemical variations along the northern portion of the Chilean Southern Volcanic Zone. In order to evaluate these hypotheses, we present a comprehensive geochemical data set (major and trace elements and O–Sr–Nd–Hf–Pb isotopes) from Holocene primarily olivine-bearing volcanic rocks across the arc between 34.5°S and 38.0°S, including volcanic front centers from Tinguiririca to Callaqui, the rear arc centers of Infernillo Volcanic Field, Laguna del Maule and Copahue, and extending 300 km into the backarc. -
Crustal Contributions to Arc Magmatism in the Andes of Central Chile
Contributions to Contrib Mineral Petrol (1988) 98:455M89 Mineralogy and Petrology Springer-Verlag 1988 Crustal contributions to arc magmatism in the Andes of Central Chile Wes Hildreth 1 and Stephen Moorbath 2 1 USGS, Menlo Park, California 94025, USA 2 Department of Earth Sciences, University of Oxford, OX1 3PR, UK Abstract. Fifteen andesite-dacite stratovolcanoes on the vol- ascending magmas, but the base-level geochemical signature canic front of a single segment of the Andean arc show at each center reflects the depth of its MASH zone and along-arc changes in isotopic and elemental ratios that dem- the age, composition, and proportional contribution of the onstrate large crustal contributions to magma genesis. All lowermost crust. 15 centers lie 90 km above the Benioff zone and 280 _+ 20 km from the trench axis. Rate and geometry of subduction and composition and age of subducted sediments and sea- floor are nearly constant along the segment. Nonetheless, Introduction from S to N along the volcanic front (at 57.5% SiO2) K20 rises from 1.1 to 2.4 wt %, Ba from 300 to 600 ppm, and Despite growing acceptance that several mantle, crustal, Ce from 25 to 50 ppm, whereas FeO*/MgO declines from and subducted reservoirs contribute to arc magmas along >2.5 to 1.4. Ce/Yb and Hf/Lu triple northward, in part continental margins, there is still no real consensus concern- reflecting suppression of HREE enrichment by deep-crustal ing the proportions of the various contributions nor con- garnet. Rb, Cs, Th, and U contents all rise markedly from cerning the loci and mechanisms of mixing among source S to N, but Rb/Cs values double northward opposite components or among variably evolved magma batches. -
Origin of Fumarolic Fluids from Tupungatito Volcano (Central Chile): Interplay Between Magmatic, Hydrothermal, and Shallow Meteoric Sources
Bull Volcanol (2013) 75:746 DOI 10.1007/s00445-013-0746-x RESEARCH ARTICLE Origin of fumarolic fluids from Tupungatito Volcano (Central Chile): interplay between magmatic, hydrothermal, and shallow meteoric sources Oscar Benavente & Franco Tassi & Francisco Gutiérrez & Orlando Vaselli & Felipe Aguilera & Martin Reich Received: 7 March 2013 /Accepted: 28 June 2013 /Published online: 25 July 2013 # Springer-Verlag Berlin Heidelberg 2013 Abstract Tupungatito is a poorly known volcano located crustal sediments. Gas geothermometry based on the kinet- about 100 km eastward of Santiago (Chile) in the northern- ically rapid H2–CO equilibria indicates equilibrium temper- most sector of the South Volcanic Zone. This 5,682 m high atures <200 °C attained in a single vapor phase at redox volcano shows intense fumarolic activity. It hosts three crater conditions slightly more oxidizing than those commonly lakes within the northwestern portion of the summit area. characterizing hydrothermal reservoirs. Reactions in the Chemical compositions of fumarolic gases and isotopic sig- H2O–CO2–H2–CO–CH4 system and C2–C3 alkenes/alkanes natures of noble gases (3He/4He and 40Ar/36Ar are up to 6.09 pairs, which have relatively slow kinetics, seem to equili- Ra and 461, respectively), and steam (δ18O and δD) suggest brate at greater depth, where temperatures are >200 °C and that they are produced by mixing of fluids from a magmatic redox conditions are consistent with those inferred by the source rich in acidic gas compounds (SO2, HCl, and HF), presence of the SO2–H2S redox pair, typical of fluids that and meteoric water. The magmatic–hydrothermal fluids are have attained equilibrium in magmatic environment. -
Descriptive Stats Craterdiam 1162Records
This electronic thesis or dissertation has been downloaded from Explore Bristol Research, http://research-information.bristol.ac.uk Author: Ituarte, Lia S Title: Exploring differential erosion patterns using volcanic edifices as a proxy in South America General rights Access to the thesis is subject to the Creative Commons Attribution - NonCommercial-No Derivatives 4.0 International Public License. A copy of this may be found at https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode This license sets out your rights and the restrictions that apply to your access to the thesis so it is important you read this before proceeding. Take down policy Some pages of this thesis may have been removed for copyright restrictions prior to having it been deposited in Explore Bristol Research. However, if you have discovered material within the thesis that you consider to be unlawful e.g. breaches of copyright (either yours or that of a third party) or any other law, including but not limited to those relating to patent, trademark, confidentiality, data protection, obscenity, defamation, libel, then please contact [email protected] and include the following information in your message: •Your contact details •Bibliographic details for the item, including a URL •An outline nature of the complaint Your claim will be investigated and, where appropriate, the item in question will be removed from public view as soon as possible. ID Sample.ID Unit.sampled Unit.filter IAVCEI.ID Volcano.ID.Number Volcano.Name 130 -99 NP Volcano and eruption