DOCSLIB.ORG

Mapa Final Prueba 2

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

SISTEMAS ELÉCTRICOS DE CHILE 2016 PRINCIPALES CIFRAS Chapiquiña Lago Chungará 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 y Gómez Río Illapel 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 Los Almendros TrebalRío Mapocho 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 MonterricoRío Ñuble San Vicente Penco 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 Río Palena Río 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”..
Recommended publications
  • Taxonomic Revision of the Chilean Puya Species (Puyoideae

    Taxonomic Revision of the Chilean Puya Species (Puyoideae

    Taxonomic revision of the Chilean Puya species (Puyoideae, Bromeliaceae), with special notes on the Puya alpestris-Puya berteroniana species complex Author(s): Georg Zizka, Julio V. Schneider, Katharina Schulte and Patricio Novoa Source: Brittonia , 1 December 2013, Vol. 65, No. 4 (1 December 2013), pp. 387-407 Published by: Springer on behalf of the New York Botanical Garden Press Stable URL: https://www.jstor.org/stable/24692658 JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at https://about.jstor.org/terms New York Botanical Garden Press and Springer are collaborating with JSTOR to digitize, preserve and extend access to Brittonia This content downloaded from 146.244.165.8 on Sun, 13 Dec 2020 04:26:58 UTC All use subject to https://about.jstor.org/terms Taxonomic revision of the Chilean Puya species (Puyoideae, Bromeliaceae), with special notes on the Puya alpestris-Puya berteroniana species complex Georg Zizka1'2, Julio V. Schneider1'2, Katharina Schulte3, and Patricio Novoa4 1 Botanik und Molekulare Evolutionsforschung, Senckenberg Gesellschaft für Naturforschung and Johann Wolfgang Goethe-Universität, Senckenberganlage 25, 60325, Frankfurt am Main, Germany; e-mail: [email protected]; e-mail: [email protected] 2 Biodiversity and Climate Research Center (BIK-F), Senckenberganlage 25, 60325, Frankfurt am Main, Germany 3 Australian Tropical Herbarium and Tropical Biodiversity and Climate Change Centre, James Cook University, PO Box 6811, Caims, QLD 4870, Australia; e-mail: [email protected] 4 Jardin Botânico Nacional, Camino El Olivar 305, El Salto, Vina del Mar, Chile Abstract.
  • Glacier Runoff Variations Since 1955 in the Maipo River Basin

    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

    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.
  • Late Pleistocene and Holocene Tephrochronology of Mendoza Province, Argentina

    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.
  • San Jose – Marmolejo

    San Jose – Marmolejo

    ANDES MOUNTAIN EXPEDICIONES - CHILE SAN JOSE VOLCANO (5.740m.) & MARMOLEJO (6.100m.) Trip. Length: 14 days San Jose volcano and Marmolejo are located into Maipo valley near Santiago Chile. Our expedition begins in Santiago airport where our guides await you at the airport. After accommodate in our hotel, we will check your personal mountaineering equipment according to our equipment list (see below). This is a very important step in the expedition, sometimes we discover some clothes not warm enough for this mountain, do not sub estimate cold temperatures in this mountain. In that case we can suggest some alternatives and also stores where you can buy or rent extra equipment. Also, we will discuss the philosophy and style of the expedition, prescription medications at altitude, the effects of Diamox (Acetazolamida), sanitation, water treatment, teamwork, techniques and advises to climbing a high mountain. At day two of our program we will transfer through Maipo Valley, a 2 hours ride from our Hotel. SAN JOSE VOLCANO Our meals are varied and well chosen. Fresh and delicious food is always available in our trips. Vegetables, fruit, meet, chicken and even fish are among our menu, as well as pastas, rice, potatoes rich in carbohydrates. Wine, coke, beer, biscuits, cheese, crackers and everything we www.andesmountain.cl [email protected] ANDES MOUNTAIN EXPEDICIONES - CHILE need to make our trip pleasant. In high camps we use intensive amount of calories per day, carbohydrates, weight, taste, variety and creativity. Approach to Base camps. San Jose BC: One day to arrive at Base camp. Horses will help us to carry our load.
  • Chile & Easter Island 11

    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 .
  • Ojos Del Salado Volcano Is the World’S Highest Active Volcano, at 6893 Meters, Well-Known for Its Impressive and Foreboding Height

    Ojos Del Salado Volcano Is the World’S Highest Active Volcano, at 6893 Meters, Well-Known for Its Impressive and Foreboding Height

    This 25-day program is made up of 19 expedition days, with rest days between expeditions. The program is subject to modification depending on weather conditions and the physical conditions and capacities of the participants. The program includes all costs related to the expedition: El Programa incluye todos los gastos relacionados a la expedición. -Transportation, logistics, food, guide, donkeys and/or porters. The program does not include hotels, transportation within the metropolitan region or Copiapó, and other costs outside of the expedition. Program: Ojos Del Salado Volcano is the world’s highest active volcano, at 6893 meters, well-known for its impressive and foreboding height. Located in the Atacama desert, near the Argentinian border, this mountain is not very technically challenging, but it’s meteorological conditions make it a great challenge for any mountaineer. This program is designed with the end goal of summiting the Ojos Del Salado Volcano, with appropriate acclimatization built in. Chronogram. The expedition begins in the mountains nearby to Santiago, Chile, Cerro El Pintor (4.180 m). This mountain is a natural lookout to Cerro El Plomo (5.424 m). This first mountain will be summited in a single day. Cerro El Pintor Our next objective is the Cerro El Plomo (5.424 m) the “apu” (guardian) of the central Mapocho valley chosen by the Incas and holds a lot historical importance. In 1954, the famous El Plomo Mummy was discovered here, at an altitude of 5,000 meters. This expedition will take us 5 days, beginning and ending in Santiago. Cerro el Plomo from El Pintor After our expedition to El Plomo, we will enter the heart of the Cajon del Maipo where we will set our sights on the most southern 6,000 meter mountains in the Andes and in the world, El Marmolejo (6,100m).This mountain neighbors Argentina, and is the tallest peak in the region, with expansive views of all of the valleys that course through the Cajón Del Maipo.
  • USGS Open-File Report 2009-1133, V. 1.2, Table 3

    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
  • Annex 36 Survey of High Mountain Activities in the San José De Maipo Commune

    Annex 36 Survey of High Mountain Activities in the San José De Maipo Commune

    ANNEX 36 SURVEY OF HIGH MOUNTAIN ACTIVITIES IN THE SAN JOSÉ DE MAIPO COMMUNE 1 INTRODUCTION The purpose of this survey is to describe the main attractions that the commune of San José de Maipo has to offer in terms of mountain activities and adventure sports. The survey, which is by no means exhaustive, is based on publicly-available information on the localities in the direct area of influence of the Project. More specifically, the information on high mountain activities in San José de Maipo needed for the survey was obtained from municipal agencies and the internet, mainly from the websites of tourist agencies operating in the area. The activities and the areas where these activities take place are discussed in the following sections. 2 MAIN ACTIVITIES The main mountain activities of the commune of San José de Maipo are: mountaineering, climbing, hiking, trekking, and skiing. In general, these activities take place in the upper basins of the Colorado, El Volcán and Yeso rivers, and include: Colorado river basin: walking, hiking, rambling, horseback riding, and adventure sports, such as mountaineering, trekking, sport climbing and traditional climbing. El Volcán river basin: walking, hiking, rambling, and adventure sports, such as mountaineering, trekking, randonee skiing, sport climbing, and traditional climbing and ice climbing. Yeso river basin: mountaineering, trekking and ice climbing. The most popular mountain peaks of the area are listed in the table below: Table 2.1 Principal Peaks of the San José de Maipo Commune Area Peak Elevation
  • South America's Premier Helicopter Skiing Operation

    South America's Premier Helicopter Skiing Operation

    South America’s Premier Helicopter Skiing Operation Welcome to Powder South Heli-Ski Guides 2 Powder South Heli-Ski Guides is South America’s premier helicopter ski operation, located in the heart of the Chilean Central Andes. Since 2002, we have been offering excellence in heli-skiing, deep in the enchanting and rugged Andes Mountain Range of Southern South America. At Powder South, we present an entirely new dimension of remote heli-skiing with world-class standards, and vast terrain for skiers and snowboarders from around the world. We offer week long and three-day packages of absolutely the best heli-skiing in the most alluring and pristine terrain the Andes has to offer with thousands of vertical feet of untouched champagne powder. Our Heli-ski packages are culturally unique and reflect the generous hospitality of the traditional Chilean mountain lodges. Our location in the Southern Hemisphere enables us to offer alternate season heli-skiing during the Northern Hemisphere summers, from June to October. 3 Founders of Powder South Powder South Heli-Ski Guides was founded by ski and mountaineering entrepreneurs and guides, Rodrigo Mujica (IFMGA/UIAGM Guide) and Joaquín Oyarzún (former Olympic Skier). Both have dedicated their lives to the mountains and to excellence in mountain guiding and adventure travel. This synergy of talents brings Powder South to the highest level of Heli-ski guiding in South America. We proudly invite you to join us in exploring fresh powder, true adventure and vertical challenge within the unsurpassed beauty of the Chilean Andes. 4 Rodrigo Mujica / Director Joaquín Oyarzún / Director An Internationally Certified UIAGM / IFMGA Executive Director and Co-Founder of Powder Mountain Guide, Director and Co-Founder of South.
  • Alto Maipo Hydroelectric Power Project Source of The

    Alto Maipo Hydroelectric Power Project Source of The

    1 ALTO MAIPO HYDROELECTRIC POWER PROJECT (1) ENVIRONMENTAL AND SOCIAL STRATEGY I. SUMMARY Country: Chile Sector: Renewable Energy - Hydropower Project name: Alto Maipo Hydroelectric Power Project Source of the deal: SCF/INF Project team: Brian Blakely, Project Team Leader (SCF/INF), Federico Lau (SCF/INF), Joana Pascual (SCF/INF), Jose Felix-Filho (VPS/ESG), Ulrike Aulestia Vargas (SCF/PMU) and Jan Weiss (SCF/SYN) Supervisor: Jean-Marc Aboussouan (Chief, SCF/INF) Borrower: Alto Maipo SPA (“Alto Maipo” or the “Borrower”) Sponsor: AES Gener S.A. (“AES Gener”) Total project cost: Approximately US$1.375 billion IDB A Loan: Up to US$[200 ]million Environmental “A” Category: II. BACKGROUND AND PROJECT DESCRIPTION Introduction 2.1 The Alto Maipo Hydroelectric Project (Proyecto Hidroeléctrico Alto Maipo – “PHAM” or “the Project”) consists of the construction and operation of two run-of- the-river hydroelectric facilities with a combined capacity of 531 MW (Alfalfal II, with a capacity of 264 MW and Las Lajas, with a capacity of 267 MW) located approximately 50 km east of Santiago, Chile (see Figures 1 and 2). The two plants will use the waters of the upper basin of the Yeso and Volcán rivers, as well as the waters of the middle and lower course of the Colorado River in the Commune or Municipality of San José de Maipo. 2.2 The PHAM will capture flow from four tributaries to the Volcán River, the Yeso River, the Aucayes Stream, and the Colorado River (via the existing Alfalfal I and Maitenes Hydropower Plants), all of which are tributaries to the Maipo River, to operate the Alfalfal II and Las Lajas powerhouses in series prior to discharging to the Maipo River.
  • Crustal Contributions to Arc Magmatism in the Andes of Central Chile

    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.