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Línea Base De Conocimientos Sobre Los Recursos Hidrológicos E Hidrobiológicos En El Sistema TDPS Con Enfoque En La Cuenca Del Lago Titicaca ©Roberthofstede
Línea base de conocimientos sobre los recursos hidrológicos e hidrobiológicos en el sistema TDPS con enfoque en la cuenca del Lago Titicaca ©RobertHofstede Oficina Regional para América del Sur La designación de entidades geográficas y la presentación del material en esta publicación no implican la expresión de ninguna opinión por parte de la UICN respecto a la condición jurídica de ningún país, territorio o área, o de sus autoridades, o referente a la delimitación de sus fronteras y límites. Los puntos de vista que se expresan en esta publicación no reflejan necesariamente los de la UICN. Publicado por: UICN, Quito, Ecuador IRD Institut de Recherche pour Le Développement. Derechos reservados: © 2014 Unión Internacional para la Conservación de la Naturaleza y de los Recursos Naturales. Se autoriza la reproducción de esta publicación con fines educativos y otros fines no comerciales sin permiso escrito previo de parte de quien detenta los derechos de autor con tal de que se mencione la fuente. Se prohíbe reproducir esta publicación para venderla o para otros fines comerciales sin permiso escrito previo de quien detenta los derechos de autor. Con el auspicio de: Con la colaboración de: UMSA – Universidad UMSS – Universidad Mayor de San André Mayor de San Simón, La Paz, Bolivia Cochabamba, Bolivia Citación: M. Pouilly; X. Lazzaro; D. Point; M. Aguirre (2014). Línea base de conocimientos sobre los recursos hidrológicos en el sistema TDPS con enfoque en la cuenca del Lago Titicaca. IRD - UICN, Quito, Ecuador. 320 pp. Revisión: Philippe Vauchel (IRD), Bernard Francou (IRD), Jorge Molina (UMSA), François Marie Gibon (IRD). Editores: UICN–Mario Aguirre; IRD–Marc Pouilly, Xavier Lazzaro & DavidPoint Portada: Robert Hosfstede Impresión: Talleres Gráficos PÉREZ , [email protected] Depósito Legal: nº 4‐1-196-14PO, La Paz, Bolivia ISBN: nº978‐99974-41-84-3 Disponible en: www.uicn.org/sur Recursos hidrológicos e hidrobiológicos del sistema TDPS Prólogo Trabajando por el Lago Más… El lago Titicaca es único en el mundo. -
Suma Qamaña Y Desarrollo El T'hinkhu Necesario
Suma Qamaña y Desarrollo El t'hinkhu necesario PPPooorrr MMMaaarrriiiooo TTTooorrrrrreeezzz EEEggguuuiiinnnooo Mario Torrez Eguino Suma Qamaña y Desarrollo El t'hinkhu necesario Edición al cuidado de Javier Medina y Simón Yampara Programa Nacional Biocultura Indice Presentación ................................... ..............................................................................9 Prólogo ................................................................................................................11 I. Urakpacha 1. Estructura y proceso de desarrollo del Qamaña. Espacio de bienestar. ...........................................................................15 2. Pacha y ecología ....................................................................................35 3. Ecología aymara: unidad e interacción de fuerzas-energías materiales-espirituales y territoriales para la qamaña, con Simón Yampara ............................41 ® Mario Torrez Eguino 4. Características rememorativas de la ecología D.L.: andina en el Qullasuyu ........................................................................55 5. Ecosistemas ...........................................................................................65 Primera Edición: Marzo 2012 II. Uñjaña Cuidados de edición: Freddy Ramos A. Foto tapa: Archivo CADA 6. El conocimiento hierático en el saber andino, con Simón Yampara .............................................................................75 Diseño de cubierta, diagramación e impresión: 7. Lógica del pensamiento andino -
Listado De Empresas (Proveedores De Articulos)
LISTADO DE EMPRESAS (PROVEEDORES DE ARTICULOS) Nro EMPRESA CODIGO TELEFONO DIRECCION 1 CAYOJA 4346C00 2225527 HEROES DEL PACIFICO N§1345 2 CONBOL 3210150 2721120-70619617 CALLE GOBLES NO.6970 DEPTO 202 3 EBA EMPRESA BOLIVIANA DE ALMENDRA Y DERIVADOS 4359W00 2146292 AV CAMACHO N§1148 4 ENTEL EMP.NAL.DE TELECOMUNICACION 420012 2141010 CALLE FEDERICO ZUAZO NO. 1771 5 LOS ANDES IMPORTACIONES Y DECORACIONES 4323I00 2462548 AV. PANDO NRO. 125 6 M.E.A.A. INDUSTRIAS 4325I00 2230169 C.INCA ALONZO 1419 VILLA SAN ANTONIO ALTO 7 MAISDA DABDOUD SCHMIEDL ISSA JEAN MAURICE 4353D00 2244305 AV TEJADA SORZANO N§606 MIRAFLORES 8 A & B INTERNACIONAL LTDA. 3210700 2432052-2434958 C. MACARIO PINILLA Nº 384 9 A&A - ARTES GRAFICAS INTEGRALES 4357M00 2419654 JAIME ZUDA¥EZ SOPOCOACHI 10 A.P.U. - ASOCIACION PRODUCTORES UNIDOS 4352B00 4734868 AV. HUMBERTO ASIN RIVERO 11 AAYSBRI 4357K00 60126840 CALLE BARBARO CASO JUAN N§ 520 12 ADM - SAO S.A. 4398600 2820307 AV JORGE CARRASCO NO. 920 Z 12 DE OCT EL AL 13 ADMI TV S.A. 4355Y00 2224422 AV. 26 DE FEBRERO VILLA SAN LUIS UV.31 MZA1 14 AFIMUR - MUEBLERIA 4348H00 2339182 CALLE MURILLO ESQ. ORURO NRO 1188 15 AGENCIA DE NOTICIAS FIDES 4100900 LA PAZ BOLIVIA 16 ALMACEN DE ABARROTES "EYNAR" 4354G00 2454281 CALLE ISAAC TAMAYO N§ 571 17 ALMACEN SANTA CRUZ - ELSA APAZA CHOQUE 4325F00 2453805 MAX PAREDES NRO 589 18 ARNULFO YUFRA ALFARO 4358P00 44319943 4319945 AV.H.DE LA INDEPENDENCIA ESQ.6 DE AGOSTO TJ 19 ARPAL - EDITORIAL IMPRENTA 4349A00 2146887 CALLE BATALLON SUCRE N§509 SAN PEDRO 20 ART OFFICE S.R.L. -
ILLIMANI and the NAZIS. E. S. G. De La Motte
ILLIMANI AND THE NAZIS ILLIMANI AND THE NAZIS BY E. S. G. DE LA MOTTE E traveller to Bolivia from Buenos Aires spends three and a half weary days in the train with no interesting scenery to relieve the monotony of his existence. He leaves the dead flat Argentine pampas, where the horizon is like the horizon at sea, and passes almost imperceptibly to the equally flat, but much more barren, high tableland of Bolivia situated at 12,ooo ft. above sea-level. There is a difference, however. This tableland runs as a relatively narrow belt for hundreds of miles between the two main Andine ranges, and therefore has the advantage over the dreary expanses of Argentina that mountains of some sort are visible from most parts of it. Nevertheless, it is with relief that towards the end of the journey the immense ice-draped mass of Illimani is seen close at hand. The height of Illimani is still uncertain, as no triangulation has yet been made of it. All those who have climbed it, however, have. taken aneroid readings and these give results varying between 20,700 ft. ·and 22,400 ft. The probability is that the lower limit is nearer the truth, so 21 ,ooo ft. may reasonably be taken as a fair approximation. In any case, whatever the exact height may be, the mountain is a singularly striking one on account of its isolation, its massive form, and its position of domination over La Paz, which is the seat of the Bolivian Government, and from many of whose houses and streets the three heavily iced summits can be seen. -
Impact of Climate Change on the Poor in Bolivia
Global Majority E-Journal, Vol. 3, No. 1 (June 2012), pp. 33-43 Impact of Climate Change on the Poor in Bolivia Christian Winters Abstract Bolivia is one of the poorest countries in South America and as a result is particularly vulnerable to climate change, which poses a threat to both the urban and rural poor. The changing weather patterns and rapid melting of glaciers in the Andes can cause both drought and flooding. That in turn will have an adverse impact on agriculture and the livelihoods of the poor. The economically vulnerable will suffer the most because of their limited ability to adapt. This article will examine the impacts of climate change in detail and will explore some of the options currently available to mitigate those impacts. I. Introduction In the heart of South America sits Bolivia, nestled between the soaring peaks of the Andes (on its west) and the Amazonian jungle (on its east). Given this location, Bolivia has a diverse geography with varied climates. It is the people in these diversities that are facing the specter of climate change in ways that not many would expect. In contradistinction with the trend of rising temperatures in the rest of the world, Bolivia’s overall temperatures have dropped, especially in the highlands. Bolivia’s changing climate is also characterized by unexpected impacts mainly on reduced cloud cover and precipitation in the highlands. It is the effect of climate change on people, specifically Bolivia’s poor and indigent, which is of capital concern. Any sudden change in the quantity of a given resource has an economic cost. -
Condoriri East Peak, Illampu West Face, and Climbs in the Apolobamba
Condoriri East Peak, Illampu West Face, and Climbs in the Apolobamba. The 1997 University of Edinburgh Apolobamba Expedition comprised Tom Bridgeland, Sam Chinnery, Rob Goodier, Jane McKay, Heather Smith and me. We spent July and August climbing in Bolivia’s Cordillera Real and the Apolobamba Range. We first went to the Condoriri area and climbed Pequeño Alpamayo (5370m) and the main summit of Condoriri (5648m) by the normal routes. Condoriri’s East Peak (Ala Derecha, 5330m) has four prominent couloirs visible from base camp. The right-hand couloir is the most obvious and was climbed by Mesili in 1976, but now appears to be badly melted out. On July 16, Sam and I climbed the narrow left-most couloir (Scottish VI/6,450m) of the four (possible second ascent). This was an excellent line, reminiscent of classic Scottish gully routes. There were three sections of vertical ice and a hard mixed section where the ice was discontinuous. We think this is probably the Couloir Colibri climbed by Gabbarou and Astier in 1989 (who reportedly found it hard). On the same day Rob and Tom climbed the second couloir (Scottish III/4, 450m) from the left (sans ropes), which was mostly névé with sections of steeper ice. It was probably a first ascent. On July 19, Jane and Heather climbed Huayna Potosi (6088m) by the normal route on the east side, while Rob, Tom, Sam and I climbed the West Face (1000m of 55° névé). Jane and Heather then climbed Illimani (6438m) by the standard route. After this Sam and I traveled to the Illampu region, and on the east side of the range we climbed, together with Jenz Richter, the Austrian Route on Pico del Norte (6045m). -
1 Recorrido Autorizado Ida Retorno
RECORRIDO AUTORIZADO Gestion 2008 Linea: 1 IDA RETORNO Macro Distrito: 2 Macro Distrito: 5 Distrito: 10 Distrito: 18 Zona: Ciudadela Ferroviaria Zona: Caliri Sale de: San Martín Sale de: Zona Caliri San Martín, Ciudadela Ferroviaria, Pura Pura, Av. Ismael Vásquez, Av. Zona Caliri, zona Bosque de Bolognia, zona Bella Vista, calle 17 de Obrajes, Manco Kapac, Av. Ildefonso de las Muñecas, Av. América, plaza Alonzo de Av. Hernando Siles, Av. Del Libertador, zona San Jorge, Av. Aniceto Arce, Mendoza, calle Bozo, plaza Pérez Velasco, San Francisco, Av. Mariscal Av. Villazón, plaza Del Estudiante, Av. 16 de Julio, Av. Mariscal Santa Cruz, Santa Cruz, Av. 16 de Julio, plaza Del Estudiante, Av. Villazón, Av. 6 de San Francisco, plaza Pérez Velasco, Av. Ismael Montes, Av. Pando, Av. Agosto, San Jorge, Av. Del Libertador, Av. Hernando Siles, calle 17 de Ildefonso de las Muñecas, plaza Eduardo Urquieta, Ex-Estación Central, Av. Obrajes, zona Bella Vista, zona Bosque de Bolognia, zona Caliri (Parada). Ismael Vásquez, Pura Pura, Ciudadela Ferroviaria, San Martín (Parada). Llega a : Zona Caliri Llega a : San Martín Tiempo estimado: 60 Min. Tiempo estimado: 60 Min. Longitud aproximada: 17 Km Longitud aproximada: 17 Km Actualmente, el operador de este recorrido es SINDICATO LITORAL, afiliada a la CENTRAL ÚNICA DE TRANSPORTE URBANO DE PASAJEROS DE LA PAZ, en la modalidad MICRO NOTA .- Opera Recorrido Autorizado por el G.M.L.P. sin costo alguno RECORRIDO AUTORIZADO Gestion 2008 Linea: 2 IDA RETORNO Macro Distrito: 1 Macro Distrito: 7 Distrito: 3 Distrito: 1 Zona: Sopocachi Zona: San Sebastián Sale de: Av. Las Kantutas Sale de: Av. -
Program the Huayna Potosi, 2 Days
Climbing Huayna Potosi (6088M) 2 days Bolivia´s Most Popular climb Huayna Potosi (6088m) is northeast of La Paz in the Cordillera Real and is known as one of the easiest 6000m plus mountains to climb in the world. Deservedly one of Bolivia’s most popular climbs and after just one hour of driving and 3 hours of walking you will be at the high camp. Huayna Potosi can be climbed by complete beginners, and provides amazing views of the Cordillera Real, Lake Titicaca (3810m) and the Altiplano (4000m). If hoping to climb higher mountains in the area, Huayna Potosi is a good starter! Program details Type of activity: Technical climbing with ropes, trekking up to high camp (5200m) Difficulty: some fitness / good fitness Experience required: no experience / some experience Grade of climb: Normal route II/AD - 50° Number of days: 2 days, 1 night Tour starts in La Paz Tour ends in La Paz Best time of year: May to September Season: Dry season: days are mild and nights are cold Highlights: learning basic ice climbing and mountaineering techniques, climbing Huayna Potosi, views of the Cordillera Real Program Day 1: La Paz (3600m) - Paso Zongo (4700m) - High camp (5200m) We drive from La Paz to Paso Zongo (4700m). From Paso Zongo we start to trek up to high camp. High camp is on a rock buttress at an altitude of 5200m and at the base of the glacier. The walk up in on a well used path on rock. Once at high camp we need to get our gear ready for the next day, as we have an early start in the morning. -
Near-Surface Faceted Crystals, Avalanches and Climate in High-Elevation, Tropical Mountains of Bolivia
Cold Regions Science and Technology 33Ž. 2001 291–302 www.elsevier.comrlocatercoldregions Near-surface faceted crystals, avalanches and climate in high-elevation, tropical mountains of Bolivia Douglas Hardy a,), Mark W. Williams b, Carlos Escobar c a Climate System Research Center and Department of Geosciences, UniÕersity of Massachusetts, Amherst, MA, 01003-9297, USA b Department of Geography and Institute of Arctic and Alpine Research, UniÕersity of Colorado, Boulder, CO, USA c BoliÕian Association of Mountain Guides, La Paz, BoliÕia Received 1 September 2000; accepted 23 July 2001 Abstract The importance of near-surface faceted crystals in forming weak layers associated with snow avalanches has recently received greater attention. However, there is still much to be learned concerning the formation and growth of these crystal types, their geographical extent, and related avalanche activity. Here we report on two avalanches that occurred during late September 1999 at high-elevations in the Bolivian Andes. Climbers released one slide at about 5200 m in the Cordillera ApolobambaŽ. on El Presidente , which claimed two lives. Four days later and 200 km to the southeast, snow scientists servicing a high-elevation meteorological site triggered another at 6300 m near the summit of IllimaniŽ. Cordillera Real . Both slab avalanches fractured through 25–50 cm of relatively new snow, with deeper pockets of wind redistributed snow. Snowpit analyses on Illimani showed the avalanche ran on a thick layer of near-surface faceted crystals overlying the austral winter dry-season snow surface. Average crystal size was 5–7 mm, and individual crystals exceeded 10 mm in diameter. We evaluate local and regional meteorological information in an effort to understand what caused the growth of these large crystals and the resultant snowpack instability. -
Bolivia 2006
ERlK MONASTERIO Bolivia 2006 Thanks are due to thejDlfowing contributors to these notes: Lindsay Griffin, John Biggar, Nick Flyvbjerg, Juliette Gehard, Arnaud Guilfaume, Moira Herring, Alain Mesili, Charlie Netherton and Katsutaka Yokoyama. Favourable weather conditions arrived early in the 2006 season with a premature end to the austral summer monsoon. As usual, most climbing activity was on the normal routes on Huayna Potosi, Illimani and Condoriri, but it was gratifying to see more trekking and climbing activity in the northern Cordillera Real, which has been quite neglected in recent years. Glacier conditions on the approaches to the western routes of Ancohuma and Illampu were by far the best seen over the past 10 years, as there were few crevasses and penitents, but the overall trend is still for rapid glacial recession. Unseasonably early snowfall arrived later in the season, substantially increasing the avalanche risk. Local guides say the climbing season is moving earlier each year. In 2005 the weather was almost continuously bad throughout September. The political situation is always important when it comes to planning a trip to Bolivia's Cordillera. The February 2006 democratic elections were unprecedented in terms of voter turnout, and for the first time elected as president an indigenous leader from a non-traditional party. Evo Morales won by a clear majority and formed a government with strong ideological affiliations to Venezuela and Cuba, rejecting US influence. This brought initial stability to the nation and the political demonstrations and strikes that in previous years paralysed the nation were not a problem during the May-September climbing season. -
Proyecto Illimani “Oferta De Agua Histórica En
Fortaleciendo la capacidad y desarrollando estrategias de adaptación a los fenómenos de Cambio Climático en comunidades de montaña de la Cordillera Real de Los Andes Centrales de Bolivia INSTITUTO DE HIDRÁULICA E HIDROLOGÍA PROYECTO ILLIMANI “OFERTA DE AGUA HISTÓRICA EN LA CUENCA DEL RÍO SAJHUAYA” INFORME FINAL Daniel R. Espinoza Romero Pablo Fuchs LA PAZ – BOLIVIA Octubre 2011 INDICE DE CONTENIDO 1 INTRODUCCIÓN _______________________________________________________________ 1 1.1 Antecedentes ______________________________________________________________ 1 1.2 Objetivo ___________________________________________________________________ 1 1.3 Contenido y alcance _________________________________________________________ 1 1.4 Área de estudio _____________________________________________________________ 1 1.4.1 Descripción regional general _____________________________________________ 1 1.4.2 Descripción local ________________________________________________________ 3 2 METODOLOGÍA ________________________________________________________________ 5 2.1 Enfoque de la investigación __________________________________________________ 5 2.2 Generación de la base de datos hidro-meteorológica ____________________________ 6 2.2.1 Recopilación de información ______________________________________________ 6 2.2.1.1 Termometría __________________________________________________________ 6 2.2.1.2 Pluviometría __________________________________________________________ 6 2.2.1.3 Otra información _______________________________________________________ -
EL GLACIAR DE CHACALTAYA (Cordillera Real, Bolivia)
LI B..... _ ....., E ERO 1998 L'INSTITUT FRANÇAIS DE RECHERCHE SCIENTIAQUE POUR LE DEVELOPPEMENT EN PERATRI N EL GLACIAR DE CHACALTAYA (Cordillera Real, Bolivia) Investigaciones glaciol6gicas (1991-1997) 1 2 B.Francou , E.Ramirei, J.Mendoza 3 4 5 J.Guereca ,, G. Miranda & L.Noriega 1üRSTOM, La Paz, Bolivia, 2 IHH (UMSA, La Paz, l301ivia),3 lGM (La Paz, Bolivia), 4 lE (UMSA, La Paz, l3olivia), SSENAMBl (La Paz. Bolivia). INDICE 1. PRESENTACION DEL PROGRAMA DE MONITOREO 1.1 Un Programa de monitoreo de glaciares extendido a los Andes Centrales 1 1.2. El programa de monitoreo en Bolivia: 1 1.3. Objetivo de este informe: 1 2. GENERALIDADES. 2 2.I. Como estudiar el funcionamiento de un glaciar? 2 2.2. El Glaciar de Chacaltaya: un glaciar ideal para un estudio 2 2.3. Caracteristicas deI Glaciar de Chacaltaya. 3 3. BALANCE DE MASA 6 3.I. Definiciones y metodologia 6 3.1.1. Balance neto especifico dei balance 6 3.1.2. Métodos de estimaci6n dei balance 6 3.1.3. Gradiente vertical dei balance, linea de equilibrio, raz6n entre el ârea de acumulaci6n y area total dei glaciar 6 3.1.4. Dinâmica dei glaciar, variaci6n de la velocidady oscilaciones dei frente 7 3.2. Sistema de medici6n para estimar el balance especifico neto deI Glaciar de Chacaltaya 8 3.2.1. Las balizas 8 3.2.2. Periodicidad de lectura de las balizas 10 3.3. El método de estimaci6n dei balance especifico neto a partir de la red de balizas. 10 3.4. Los resultados dei balance neto especifico a nivel anual 11 3.5.