DOCSLIB.ORG

Sistemas Eléctricos De Chile 2016

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Sistemas Eléctricos De Chile 2016 SISTEMAS ELÉCTRICOS DE CHILE 2016 PRINCIPALES CIFRAS á Chapiquiña Lago Chungar Quiani Pukará Río Lluta Parinacota Chinchorro Arica CD. Arica El Águila Potencia Neta Arica Vitor Pampa Camarones Río de Camarones Eólica________ 1.034,5 MW Dolores Solar ________ 1.216,9 MW Pacíco PAS II y III Iquique Cerro Colorado Hidráulica _____ 6.613,8 MW CD. Iquique Iquique HMC CD. Zofri Pozo Almonte CD. Estandartes Palatos La Huayca II Cerro Dragón Térmica _____ 12.862,2 MW Hospicio Tamarugal Cóndores Tarapacá Tarapacá TOTAL: 21.727,5 MW Ujina Quebrada Blanca Collahuasi Nueva Victoria Río Loa Lagunas Río Loa PEQ Líneas de Transmisión El Abra Radomiro Tomic María Elena Crucero Tensión Longitud Barriles La Cruz Norgener Salar Tocopilla Chuquicamata 500 kV 1.596,6 km El Loa CD. Tamaya Ministro Hales Encuentro 345 kV 408,0 km Antucoya Calama Valle de los Vientos Finis Terrae Jama Guayaques Río Loa 220 kV 16.739,7 km Muelle Spence Cochrane Angamos Kapatur Sierra Gorda 154 kV 1.502,8 km Andina El Tesoro Hornitos Chacaya Mejillones Atacama Esperanza 110 kV 5.847,2 km CD. Enaex Lomas Bayas El Cobre Changos Gaby Capricornio Oeste Minsal >=33 y Mantos Blancos Laberinto Desalant Antofagasta La Portada Atacama < de 110 kV 5.800,4 km Antofagasta Esmeralda O`Higgins Andes Solar Centro Uribe Sur Llanos Zaldívar Andes La Negra El Negro Palestina SVC Domeyco TOTAL: 31.894,7 km Coloso Alto Norte CD. Aguas Blancas Cobos * Suma total de largos por circuitos Escondida Salta P. Óxidos Sulfuros Nueva Zaldívar OGP 1 Laguna Seca Domeyko Paposo Taltal Parque Eólico Taltal TAP Taltal Lalackama I y II Taltal Pampa Conejo Norte Cachiyuyal Francisco Las Luces Planta Óxido Diego de Javiera Almagro Cumbres Salvador Pilar Los Amarillos Chañares Emelda D. de Chañaral Almagro El Salvador Llanta El Salado Andes San Lorenzo Potrerillos Diego de Almagro Generación Manto Verde Bombeo II Bombeo I Carrera Pinto La Coipa Totoralillo Carrera Pinto Luz del Caldera Norte San Andrés Copiapó Galleguillos Impulsión Llano de Planta Matta Hernán Fuentes Llampos Fundición Paipote Copiapó Cardones Cenizas Cardones Atacama Kosan Nueva Cardones Magnetita Tierra Amarilla Minera Maricunga Cardones Copayapu Minera Ojos del Salado Castilla Termopacíco Cerrillos Chuschampis Los Loros Las Terrazas Los Colorados Los Loros Maitencillo Punta Toro Caserones Guacolda Jorquera Huasco TG Nueva Agrosuper Pellets Maitencillo Vallenar Algarrobo Alto del Carmen Río Huasco Dos Amigos San Juan Incahuasi Santa Cecilia Punta Colorada La Silla Lama Punta Colorada Las Quebradas Punta Colorada Romeral Pan de Azúcar Las Compañías Coquimbo San Joaquín Sol Luna Guayacán Marquesa San Juan N. Pan de Azúcar Puclaro Vicuña El Peñon Tambo Real Andacollo SDGx01 Las Piedras Minera TECK La Chapeana REGIÓN DE El Arrayán Río Limarí La Paloma Don Goyo Monte Patria VALPARAÍSO Talinay Poniente Ovalle Isla Talinay Oriente Las Mollacas Los Cururos Embalse La Los Molles San Félix Punitaqui Paloma Monte Redondo El Divisadero Isla El Sauce San Ambrosio Punta Palmeras Combarbalá Loma Los Colorados Canela I PSF Casas Blancas Canela II Totoral I y II Las Palmas Isla Salas ío Illapel y Gómez R Illapel Chuchiñi Salamanca Bellavista Los Espinos Mauro Los Piuquenes Choapa Tap Mauro Los Vilos Olivos REGIÓN DE VALPARAÍSO Nogales Quereo Sta. Julia Isla de Pascua Quinquimo Casas Viejas Cabildo Marbella Campiche Nueva Ventanas Blanco Ventanas Tomaval S. Andes Hanga Roa Los Quilos Juncal Quintero Bio Cruz Chacabuquito Juncalito Los Vientos Hornitos Colmito Las Vegas S. Felipe Concón Nehuenco Aconcagua San Isidro Chagres Saladillo Torquemada Esperanza Los Maquis Mina REGIÓN DE Marga Marga San Luis Los Colorados I y II Cordillera Quillota VALPARAÍSO Miraores Quilapilun SAG Agua Santa San Pedro Polpaico Isla Robinson Valparaíso Valparaíso Tiltil Crusoe Placilla y Polpaico Sta. Filomena Conuencia Laguna Verde Curauma Las Tortolas Los Maitenes Lo Aguirre Quintay El Molle El Salto Araucarias Renca Santiago Algarrobo Norte Casablanca Iy II La Hermita San Jerónimo N. Renca Cerro Navia Isla Santa Clara Las Piñatas ío Mapocho Los Almendros TrebalR Ochagavía T. Altamira El Totoral Mapocho Santa Florida Chena Marta Florida I, II y III San Sebastián Leyda CMPC Alfalfal San Antonio Cordillera El Rincón Alto Melipilla Carena Lo Prado Maipo Maitenes Puntilla Río Maipo Mallarauco Eyzaguirre -El Llano Bajo Melipilla Buin Las Vertientes Alto Jahuel Isla Paine Los Morros Alejandro Mandinga Tissue Guayacán Selkirk Las Arañas Hospital Aux. del Maipo El Peumo Queltehues Los Bajos Rapel San Francisco Ucuquer I y II Quelentaro Alhué Energía Candelaria Volcán Rancagua Las Pampas Pacíco ARCHIPIÉLAGO Punta de Cortés Interconexión Colón JUAN FERNÁNDEZ Portezuelo Rancagua Cordillera Marchigüe Sta. Irene Lo Miranda Cachapoal Alcones Malloa N. Río Cachapoal Chacayes Paniahue Colihues Coya Nancagua San Vicente TT. Pelequén Sauzal Placilla Sauzalito San Fernando La Higuera San Andrés Chimbarongo La Conuencia Ranguili Licantén Teno El Paso Hualañé Rauquén Parronal Curicó Tinguiririca Río Mataquito Villa Prat Molina Purísima CBB-Centro El Galpón Constitución 1 Lircay Cumpeo Itahue Maule Constitución Los Maquis Mariposas Viñales Panguilemo Providencia Talca Celco Talca Maule San Clemente Chiburgo Río Maule Piduco San Clemente Curillinque Nirivilo Cipreses San Javier Ojos de Agua San Ignacio Isla Pehuenche Linares Colbún Los Hierros I y II Panimávida Machicura Loma Alta Ancoa Longaví La Vega Roblería Laguna del Maule Cauquenes Retiro Parral San Gregorio Quirihue Tap Ñiquén Coelemu San Carlos Tomé Hualte Cocharcas Concepción Talcahuano Lirquén Sta. Elvira Chillán MonterricoR San Vicente Penco ío Ñuble Newen - Petropower Perales Tres Esquinas Nva. Aldea Itata Concepción Hualpén Los Pinos - Sta. Lidia Cholguán Charrúa A. Rivera Loma Colorada Cabrero Lagunillas Chiguayante Quilleco Masisa Bocamina I y II Coronel Sta. María Laja Yungay Rucue El Toro Las Peñas Los Guindos El Manco Santa Fé Antuco Carampangue Horcones La Esperanza Cuel Los Angeles Duqueco Abanico Arauco Bureo - Munilque Mampil Buenos Aires JCE Lago Laja Negrete Ancalí I Peuchén Curanilahue CMPC Pacíco Lleuquereo Los Padres Mulchén Nahuelbuta Tres Pinos Renaico Lebu Alto Renaico Cañete Río Picoiquén Angostura El Mirador Raki Cañete Quillaileo Pangue Angol Huajache Collipulli Mulchén Ralco Contulmo Zona de caida Palmucho Los Sauces I y II Curacautín El Agrio Traiguén Victoria Tirúa Lautaro Lautaro Lonquimay Temuco Eagon Pillanlelbún Lousiana Pacic Temuco Pumahue Chivilcán El Canelo Río Trueno Padre Las Casas El Manzano Trufultruful Nueva Imperial Río Toltén Río Imperial Licanco Carilafquén Malalcahuello Cautín Pitrufquén Río Toltén Allipén Gorbea Trailelfu Maisan Donguil Pucón Molinera Villarrica Loncoche Lousiana Pacic Pullinque Ciruelos Chumpullo Mariquina Panguipulli Valdivia Calle Calle Valdivia Valdivia Los Lagos Corral Reca Picarte Paillaco Antilhue Pichirropulli Las Flores Río Bueno Muchi Doña Hilda Curileufu Pichilonco Don Walterio Chuyaca La Unión Rucatayo Pehui Watt I y II El Arrayan Pilmaiquén Licán Skretting Pilauco Osorno Los Corrales I y II Los Tambores Antillanca Chanleufu Rahue Barro Blanco Aihuapi Los Negros Pulelfu Pichil Capullo Río Bonito Callao Nalcas Los Colonos Hidrobonito I y II Purranque Frutillar Puerto Varas Ensenada Puerto Montt El Canelo I Melipulli MultiExport I y II Canutillar Molinos Trapén Cochamó Puerto Montt El Empalme Colaco La Arena Punta Barranco Calbuco Punta San Gallán Ancud Danisco Hornopirén Biomar Cuchildeo Chiloé Degañ San Pedro Dalcahue Dalcahue Pid Pid Castro Castro Dongo Chonchi Collil Chaitén Quellón Quellón I y II Chiloé Futaleufú Río Azul Palena ío Palena R R ío Palena La Junta Lago Verde Puyuhuapi Nuevo Reino Amengual El Toqui Manihuales Aysén Aysén Alto Baguales Chacabuco Coyhaique Tehuelche Lago Atravesado Monreal Puerto Ibañez Chile Chico Lago General Carrera El Traro Cochrane SIMBOLOGÍA Central Hidroeléctrica Central Termoeléctrica Central Eólica Central Solar “ACUERDO ENTRE LA REPÚBLICA DE CHILE Y LA REPÚBLICA ARGENTINA PARA PRECISAR EL RECORRIDO DEL LÍMITE DESDE EL MONTE FITZ ROY Línea 500 kV HASTA EL CERRO DAUDET” (Buenos Línea 345 kV Aires, 16 de diciembre de 1998). Línea 220 kV Línea 154 kV Línea 110 kV Línea 66 kV y menores Línea 500 kV en construcción Línea 220 kV en construcción TERRITORIO CHILENO ANTÁRTICO Nudo principal Subestación 90º 53º Puerto Natales Puerto Natales Este mapa es esquemático, las distancias y ubicaciones pueden no corresponder, en algunas ocasiones, a las reales. Actualizado a agosto de 2016 Referencias: Cabo Negro - Sistema Interconectado Norte Grande (Fuente: www.cdecsing.cl, CNE, Ministerio de Energía). Tres Puentes - Sistema Interconectado Central Punta Arenas (Fuente: www.cdecsic.cl). Punta Arenas Porvenir - Sistemas Medianos de Los Lagos Porvenir (Fuente CNE, Ministerio de Energía http://sig.minenergia.cl ). - Sistemas Medianos de Aysén (Fuente CNE, Ministerio de Energía http://sig.minenergia.cl/sig-minen/). - Sistemas Medianos de Magallanes (Fuente CNE, Ministerio de Energía http://sig.minenergia.cl/sig-minen/). Puerto Williams Puerto Williams “Autorizada su circulación, por resolución Nº135 del 20 de octubre de 2016 de la Dirección Nacional de Fronteras y Límites del Estado. La edición y circulación de mapas, cartas geográcas u otros impresos y documentos que se reeran o relacionen con los límites y fronteras de Chile, no comprometen, en modo alguno, al Estado de Chile, de acuerdo con el Artículo 2º, letra g) del DFL Nº 83 de 1979 del Ministerio de Relaciones Exteriores”..
Load more

Recommended publications
  • 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.
    [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]
  • Trekking Desolacion Trail. Volcán Osorno, Petrohué Falls,Emerald Lake. Trekking : Vicente Perez Rosales N.Park
    Trekking Desolacion trail. Volcán Osorno, Petrohué falls,Emerald Lake. Trekking : Vicente Perez Rosales N.Park. Desolation Pass. Overview: Profile: Adventurous Difficulty level: medium. Season: November to late March Other trips you might find interesting: Solitario Hike Parque Nacional V, Perez Rosales. Cochamo Walls and river Hike, Tagua Tagua Hike. We depart early in mornig from Puerto Varas to Petrohué on the shores of Todos Los Santos Lake. On our way to the lake, we’ll pass through areas that are the mouths of the rivers which flow from the sides of Osorno Volcano. On warm days, it is possible to see what appear to be dust clouds arising from the flanks of the volcano. In reality, these are ash clouds raised by the flowing waters making their way down the flanks of the volcano. We will cross vast areas of black ash mixed with the lashes from the Calbuco eruption in 2015 and have been brought down by the glacial melt. You will appreciate the might of the volcano as you see the results of the ash flows experienced during its eruptions. One can only imagine what it must have been like during its periods of activity. Leaving Petrohué, we head upward toward the base of Volcano Osorno (8,730 feet). Our trek takes us through Osorno’s volcanic canyons where amazing rock formations are etched out of the canyon walls by the melting snows and glaciers of Osorno. As we head upwards to Desolation Pass, at an altitude of 5,610 feet between the Osorno and Cerro La Picada volcanoes, we will also see a wide variety of lava formations created by the lava flows that built Osorno.
    [Show full text]
  • Volcanes Cercanos Volcanes Cercanos
    Localidades al interior de un radio de 30 km respecto de volcanes activos Volcanes cercanos Localidad Comuna Provincia Región Olca, Irruputuncu Collaguasi Pica Iquique Tarapacá Taapaca, Parinacota Putre Putre Parinacota Tarapacá Callaqui, Copahue Ralco Santa Bárbara Bio Bio Bio Bio Nevados de Chillán Recinto Los Lleuques Pinto Ñuble Bio Bio Villarrica, Quetrupillán, Lanín, Sollipulli Curarrehue Curarrehue Cautín La Araucanía Llaima, Sollipulli Mellipeuco Melipeuco Cautín La Araucanía Villarrica, Quetrupillán, Lanín Pucón Pucón Cautín La Araucanía Llaima Cherquenco Vilcún Cautín La Araucanía Villarrica Lican Ray Villarrica Cautín La Araucanía Villarrica Villarrica Villarrica Cautín La Araucanía Llaima, Lonquimay Curacautín Curacautín Malleco La Araucanía Llaima, Lonquimay Lonquimay Lonquimay Malleco La Araucanía Villarrica, Quetrupillán, Lanín, Mocho Coñaripe Panguipulli Valdivia Los Rios Calbuco, Osorno Alerce Puerto Montt Llanquihue Los Lagos Calbuco, Osorno Las Cascadas Puerto Octay Osorno Los Lagos Chaitén, Michinmahuida, Corcovado Chaitén Chaitén Palena Los Lagos Hornopirén, Yate, Apagado, Huequi Rio Negro Hualaihue Palena Los Lagos Localidades al interior de un radio de 50 km respecto de volcanes activos Volcanes cercanos Localidad Comuna Provincia Región Olca, Irruputuncu Collaguasi Pica Iquique Tarapacá Taapaca, Parinacota Putre Putre Parinacota Tarapacá San José San Alfonso San José de Maipo Cordillera Metropolitana San José San José de Maipo San José de Maipo Cordillera Metropolitana Tupungatito La Parva Lo Barnechea Santiago
    [Show full text]
  • A Review of the Current State and Recent Changes of the Andean Cryosphere
    feart-08-00099 June 20, 2020 Time: 19:44 # 1 REVIEW published: 23 June 2020 doi: 10.3389/feart.2020.00099 A Review of the Current State and Recent Changes of the Andean Cryosphere M. H. Masiokas1*, A. Rabatel2, A. Rivera3,4, L. Ruiz1, P. Pitte1, J. L. Ceballos5, G. Barcaza6, A. Soruco7, F. Bown8, E. Berthier9, I. Dussaillant9 and S. MacDonell10 1 Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA), CCT CONICET Mendoza, Mendoza, Argentina, 2 Univ. Grenoble Alpes, CNRS, IRD, Grenoble-INP, Institut des Géosciences de l’Environnement, Grenoble, France, 3 Departamento de Geografía, Universidad de Chile, Santiago, Chile, 4 Instituto de Conservación, Biodiversidad y Territorio, Universidad Austral de Chile, Valdivia, Chile, 5 Instituto de Hidrología, Meteorología y Estudios Ambientales (IDEAM), Bogotá, Colombia, 6 Instituto de Geografía, Pontificia Universidad Católica de Chile, Santiago, Chile, 7 Facultad de Ciencias Geológicas, Universidad Mayor de San Andrés, La Paz, Bolivia, 8 Tambo Austral Geoscience Consultants, Valdivia, Chile, 9 LEGOS, Université de Toulouse, CNES, CNRS, IRD, UPS, Toulouse, France, 10 Centro de Estudios Avanzados en Zonas Áridas (CEAZA), La Serena, Chile The Andes Cordillera contains the most diverse cryosphere on Earth, including extensive areas covered by seasonal snow, numerous tropical and extratropical glaciers, and many mountain permafrost landforms. Here, we review some recent advances in the study of the main components of the cryosphere in the Andes, and discuss the Edited by: changes observed in the seasonal snow and permanent ice masses of this region Bryan G. Mark, The Ohio State University, over the past decades. The open access and increasing availability of remote sensing United States products has produced a substantial improvement in our understanding of the current Reviewed by: state and recent changes of the Andean cryosphere, allowing an unprecedented detail Tom Holt, Aberystwyth University, in their identification and monitoring at local and regional scales.
    [Show full text]
  • Boron and Other Trace Element Constraints on the Slab-Derived Component in Quaternary Volcanic Rocks from the Southern Volcanic Zone of the Andes
    Geochemical Journal, Vol. 47, pp. 185 to 199, 2013 Boron and other trace element constraints on the slab-derived component in Quaternary volcanic rocks from the Southern Volcanic Zone of the Andes HIRONAO SHINJOE,1* YUJI ORIHASHI,2 JOSÉ A. NARANJO,3 DAIJI HIRATA,4 TOSHIAKI HASENAKA,5 TAKAAKI FUKUOKA,6 TAKASHI SANO7 and RYO ANMA8 1Tokyo Keizai University, Japan 2Earthquake Research Institute, The University of Tokyo, Japan 3Servicio Nacional de Geología y Minería, Chile 4Kanagawa Prefectural Museum of Natural History, Japan 5Department of Earth and Environmental Sciences, Graduate School of Science and Technology, Kumamoto University, Japan 6Department of Environment Systems, Faculty of Geo-environmental Science, Rissho University, Japan 7Department of Geology and Paleontology, National Museum of Nature and Science, Japan 8Integrative Environmental Sciences, Graduate School of Life and Environmental Sciences, Tsukuba University, Japan (Received April 18, 2012; Accepted December 25, 2012) We present a dataset for boron and other trace element contents obtained from samples from 13 volcanoes distributed along the Quaternary volcanic front of the Southern Volcanic Zone (SVZ) of the Chilean Andes. The dataset shows con- straints on the nature of slab-derived component to mantle source. Analyzed samples show large negative Nb and Ta anomalies, and enrichment of alkaline earth elements and Pb, which are features of typical island arc volcanic rocks. Boron contents of SVZ volcanic rocks range 2.3–125.5 ppm, exhibiting marked enrichment relative to N-MORB and OIB. Both the boron contents and B/Nb ratios of the volcanic rocks increase from the southern SVZ (SSVZ) to central SVZ (CSVZ). Fluid mobile/immobile element ratios (B/Nb, Ba/Nb, Pb/Nb, and K/Nb) are used to examine slab-derived com- ponent to mantle source.
    [Show full text]
  • Processes of Policy Mobility in the Governance of Volcanic Risk
    1 Processes of Policy Mobility in the Governance of Volcanic Risk Graeme Alexander William Sinclair Lancaster Environment Centre Lancaster University Lancaster LA1 4YQ UK Submitted 2019 This thesis is submitted for the degree of Doctor of Philosophy. 2 Statement of Declaration I hereby declare that the content of this PhD thesis is my own work except where otherwise specified by reference or acknowledgement, and has not been previously submitted for any other degree or qualification. Graeme A.W. Sinclair 3 Abstract —National and regional governments are responsible for the development of public policy for volcanic risk reduction (VRR) within their territories. However, practices vary significantly between jurisdictions. A priority of the international volcanological community is the identification and promotion of improved VRR through collaborative knowledge exchange. This project investigates the role of knowledge exchange in the development of VRR. The theories and methods of policy mobility studies are used to identify and explore how, why, where and with what effects international exchanges of knowledge have shaped this area of public policy. Analyses have been performed through the construction of narrative histories. This project details the development of social apparatus for VRR worldwide, depicted as a global policy field on three levels - the global (macro) level; the national (meso) level; and at individual volcanoes (the micro level). The narratives track the transition from a historical absence of VRR policy through the global proliferation of a reactive 'emergency management' approach, to the emergence of an alternative based on long-term planning and community empowerment that has circulated at the macro level, but struggled to translate into practice.
    [Show full text]
  • Dressing the Leader, Dressing the Ancestor: the Longue Durée in the South Central Andes Ann H
    University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Textile Society of America Symposium Proceedings Textile Society of America 2014 Dressing the Leader, Dressing the Ancestor: The longue durée in the South Central Andes Ann H. Peters University of Pennsylvania, [email protected] Follow this and additional works at: http://digitalcommons.unl.edu/tsaconf Part of the Art Practice Commons, and the Fiber, Textile, and Weaving Arts Commons Peters, Ann H., "Dressing the Leader, Dressing the Ancestor: The longue durée in the South Central Andes" (2014). Textile Society of America Symposium Proceedings. 945. http://digitalcommons.unl.edu/tsaconf/945 This Article is brought to you for free and open access by the Textile Society of America at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Textile Society of America Symposium Proceedings by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Dressing the Leader, Dressing the Ancestor: The longue durée in the South Central Andes Ann H. Peters The preservation and adornment of the dead in the South Central Andes can be traced over some twelve thousand years. The nature of social and political ancestry and its relationship to power change over time with the development of large-scale complex societies. These changes are reflected in the types of garments used to dress the outside of mortuary bundles and their references to socio-political roles and associations. Archaeology has barely begun to develop the analytic approaches to take advantage of textile analysis in order to reconstruct – or theorize – multifaceted identities, networks of social and political relationships, and production and exchange practices embedded in particular environments.
    [Show full text]
  • Centro Comercial Metro
    271,500 PARQUE 272,000 ELMER FAUCETT CENTRO COMERCIAL PQ. CAP. MANUEL METRO GALINDO (Auxiliar de la av. venezuela) Falco Manuel Tnte. Ca. Pje. Cap. Manuel Galindo Manuel Cap. Pje. Ca. Tnte. Juan Balcazar Ca. Teniente Eliseo Calmet San Nicolas San -U-RVp0DUtD0RUHOORV -U-RVp0DUtD0RUHOORV Pje. Bahia de Salinas de Bahia Pje. PQ. JOSE Pje. Bahia de Paracas PQ. DE LA MARIA Ca. Tnte. Enrique de Guimaraes PQ. Pje. Fogonero Isidro Alcibar Isidro Fogonero Pje. SOLIDARIDAD MORELLOS RESIDENCIAL PQ. Huarmey de Bahia Ca. FAUCETT FOGONERO 3MH%DKtDGHOD,QGHSHQGHQFLD 3MH%DKtD6DQ-XDQ Jr. Lautaro Jr. Pje. Pto. Lagunas 3MH%DKtDGH Pje. Bahia de Huacho de Bahia Pje. AV. PIO XII Pje. Bahia de Salinas de Bahia Pje. Ca. Fogonero Isidro Alcibar Isidro Fogonero Ca. AV. PIO XII Ca. Montecarlo Pje. Ampay Pje. Ca. Miguel Hidalgo Ca. Marinero Aparicio Robles Pje. Punta Zarate Punta Pje. Pje. Marinero Aparicio Robles PARQUE TRADICIONES DE RICARDO PALMA PQ. CAP. APARICIO ROBLES Lautaro Jr. Pje. Punta Sal -U-RVp0DUWL Pje. Punta Brava Punta Pje. PQ. PUNTA Ampay Ca. BOLSA BRAVA ESTACIONAMIENTO Pje. Punta Restin Jr. Cuauthemoc Jr. La Apacheta Jr. Cuauthemoc &D$xDTXLWR Pje. Punta Hermosa Punta Pje. Ca. Tutupaca Ca. Ca. Taquitahuana Ca. Camilo Carrillo Camilo Pje. Punta Balcones 3MH3XQWD3HxD1HJUD Jr. Paso de los Andes Jr. Paso de los Andes Jr.Pacamarca Pje. Punta Malpelo Ca.Huancauri AV. DE LOS INSURGENTES LOS DE AV. PQ. AV. ELMER FAUCETT PUNTA MALPELO Psj.Taquitahuana Jr. Capitan de Navio de Capitan Jr. 3MH3XQWD3DULxDV Ca. Quiquijana PQ. JOSE SANTOS CHOCANO Ca. Coropuna 8'665,500 Ca. Cap. de Navio German Stiglich Ca.
    [Show full text]
  • Indirect Tephra Volume Estimations Using Theorical Models for Some Chilean Historical Volcanic Eruptions with Sustained Columns J.E
    Indirect tephra volume estimations using theorical models for some Chilean historical volcanic eruptions with sustained columns J.E. Romero*1,2 , J.G. Viramonte 3 & R. A. Scasso 4 (1) Universidad de Atacama, Departamento de Geología. Copayapu 485, Copiapó. (2) Proyecto Archivo Nacional de Volcanes, www.archivonacionaldevolcanes.cl (3) INENCO – GEONORTE Universidad Nacional de Salta-CONICET, Av. Bolivia 5150–4400, Salta , Argentina (4)IGeBA-CONICET, Universidad de Buenos Aires, Departamento de Ciencias Geológicas, Int. Guiraldes 2160, C1428EHA, Ciudad Universitaria, Pab. II, Buenos Aires, Argentina. * Presenting Author’s email: [email protected] Introduction During explosive volcanic eruptions, diverse pyroclastic products are discharged from an eruptive column. Those columns are divided into three zones; 1) a basal gas thrust one, 2) medial convective and 3) a top umbrella region (Sparks, 1986) as is indicated in figure 1a. In this last one, where the column is dispersed laterally and radially forming a dispersion cloud or volcanic plume, the column reaches an Ht region due its momentum (Fig.1a). There has been defined two types of eruptive columns in relation with the time between single explosions. If the time between explosions exceeds the time of ascension of a column until its Ht height, the column is thermal, and in the opposite case, if the ascension time is smaller than the separation between explosions, this column is sustained (Sparks, 1986; Carey and Bursik, 2000). A good agreement has been found in the prediction of column heights and field observations for the case of columns which extends higher than the tropopause (Settle, 1978; Wilson et al, 1978; Sparks and Wilson, 1982; Sparks, 1986).
    [Show full text]
  • Challenges in Ascertaining the Late Quaternary Tephrostratigraphy of Southernmost Chile and Argentina Stefan M
    Challenges in ascertaining the late Quaternary tephrostratigraphy of southernmost Chile and Argentina 1 1 2 1 1 3 Stefan M. Lachowycz , Karen Fontijn , Victoria C. Smith , David M. Pyle , Tamsin A. Mather , José A. Naranjo [1] Department of Earth Sciences, University of Oxford, UK [2] Research Laboratory for Archaeology and the History of Art, University of Oxford, UK [3] Servicio Nacional de Geología y Minería, Santiago, Chile [email protected] # ## ! Overview Palaeoenvironmental archives 76°W 74°W 72°W 70°W 68°W 80°W 60°W 40°W Tephra preservation in palaeoenvironmental records Cha1 ! # 10°N ! Cha2 ! ! - The explosive eruption history and tephrostratigraphy in southernmost Chile/Argentina Minchinmávida Mic1 Issues with using tephra in palaeoenvironmental archives in this region to correlate records and constrain eruption parameters: and explosive eruption history ! # 0° ! Chaitén# Cor3 is significant for volcanic hazard assessment and as a tool to correlate and date reliably Corcovado# ! - 19 volcanic centres are thought to have been Cha2008 10°S Environment Physical preservation Chemical preservation Dating and record bias issues the many palaeoenvironmental archives here, but is currently poorly constrained. Yanteles# active in post-glacial times in southernmost # Yan1 Peat - Spatially and temporally variable - Al, Fe, alkali and alkali earth metals - Tephra layers are dispersed by root growth, 20°S 14 6 - We have reviewed the existing late Quaternary tephrostratigraphic record, and here # accumulation rates (F6, F7) ca use depth
    [Show full text]
  • Plan Regulador Comunal De Purranque Región De Los Lagos
    ILUSTRE MUNICIPALIDAD DE PURRANQUE PLAN REGULADOR COMUNAL DE PURRANQUE REGIÓN DE LOS LAGOS EVALUACIÓN AMBIENTAL ESTRATÉGICA INFORME AMBIENTAL ABRIL 2019 PLAN REGULADOR COMUNAL DE PURRANQUE PROFESIONAL RESPONSABLE ……………………………………………………… Maximiliano Salazar Palomo, Ingeniero Civil Geógrafo Abril 2019 PLAN REGULADOR COMUNAL DE PURRANQUE ÍNDICE DE CONTENIDOS 1. RESUMEN EJECUTIVO ......................................................................................................................... 1-1 2. ACERCA DEL PLAN REGULADOR COMUNAL .................................................................................... 2-1 2.1 OBJETIVOS DEL PLAN ........................................................................................................................ 2-1 2.1.1. Objetivo General ....................................................................................................................... 2-1 2.1.2. Objetivos de planificación .......................................................................................................... 2-1 2.2 JUSTIFICACIÓN DE LA FORMULACIÓN DEL PLAN .......................................................................... 2-2 2.3 OBJETO DE EVALUACIÓN .................................................................................................................. 2-2 2.4 ÁMBITO TEMPORAL Y TERRITORIAL DE APLICACIÓN ................................................................... 2-3 3. POLÍTICAS DE DESARROLLO SUSTENTABLE Y MEDIO AMBIENTE ...............................................
    [Show full text]