Gipfeltrekking Tocllaraju, 6034M
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Cordillera Blanca : Glaciares En La Historia
Bull. Inst. Fr. &tildes andines 36 B. FRANCOU, P. RlBSTElN - 1995, 24 (1): 37-64 THOMPSON, L.G., 1992- Ice core evidence from Peru and China. in :Clirrrnte sir~eA.D.1500.(R. Bradley and P.D. Jones editors) :517-548, London: Routledege. THOMPSON, L.G., MOSLEY-THOMPSON, E. C MORALES ARNAO, B., 1984 - El Niiio Southern Oscillation events recorded in the stratigraphy of the Tropical Quelccaya ice cap, Peru. Science, :50-53. 22 M. THOMPSON,J., L.G., MOSLEY-THOMPSON, E., DAVIS, M., LIN, P.N., YAO,T., DYURGEROV, & DAI, 1993- ”Recent warming” : ice core evidence from tropical ice cores with empllass on Central Asia. Globnl nird Plnrv&?ry Clrnqe, 7 : 145-156. CORDILLERA BLANCA GLACIARES EN LA HISTORIA I I *O Resumen Seminario internacional: La mis vasta cobertura glaciar situada entre los trilpicos aqarece como objeto de estudio AIUSE ESTRUCTURAL, POL“ AGRARIASY SECTOR AGROPECUARIO EN BOUMA, CHILE, ECUADOR Y PERU, rela tivainente tarde, a fines del sigla XIX, sobre todo gracias a Ias expediciones austro alemanas a partir organizado por el CEPES y FAO y realizado en mayo de 1994 en la ciudad de Lima. de los aiios 1930-1940.EI desarrollo del alpinismo y un gran nilmero de catistrofes mortales asociadas a la dinimica de estos glaciares (rotura de lagunas de represa morrénica, avalanchas) atrajeron la Ajuste estructural el papel relativo del sector agrario en el desarrollo del PerídJuvier lgiiifiíí y atención ysuscitaron investigaciones glaciológicas.En 1980,seencuentran entre losmejormonitoreados de losglaciares tropicales,primero, gracias a un programa -
Multi-Source Glacial Lake Outburst Flood Hazard Assessment and Mapping for Huaraz, Cordillera Blanca, Peru
ORIGINAL RESEARCH published: 21 November 2018 doi: 10.3389/feart.2018.00210 Multi-Source Glacial Lake Outburst Flood Hazard Assessment and Mapping for Huaraz, Cordillera Blanca, Peru Holger Frey 1*, Christian Huggel 1, Rachel E. Chisolm 2†, Patrick Baer 1†, Brian McArdell 3, Alejo Cochachin 4 and César Portocarrero 5† 1 Department of Geography, University of Zurich, Zurich, Switzerland, 2 Center for Research in Water Resources, University of Texas at Austin, Austin, TX, United States, 3 Mountain Hydrology and Mass Movements Research Unit, Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf, Switzerland, 4 Autoridad Nacional del Agua – Unidad de Glaciología y Recursos Hídricos (ANA-UGRH), Huaraz, Peru, 5 Área Glaciares, Instituto Nacional de Investigación Edited by: en Glaciares y Ecosistemas de Montaña (INAIGEM), Huaraz, Peru Davide Tiranti, Agenzia Regionale per la Protezione The Quillcay catchment in the Cordillera Blanca, Peru, contains several glacial lakes, Ambientale (ARPA), Italy including Lakes Palcacocha (with a volume of 17 × 106 m3), Tullparaju (12 × 106 m3), Reviewed by: 6 3 Dhananjay Anant Sant, and Cuchillacocha (2 × 10 m ). In 1941 an outburst of Lake Palcacocha, in one of Maharaja Sayajirao University of the deadliest historical glacial lake outburst floods (GLOF) worldwide, destroyed large Baroda, India Fabio Matano, parts of the city of Huaraz, located in the lowermost part of the catchment. Since Consiglio Nazionale Delle Ricerche this outburst, glaciers, and glacial lakes in Quillcay catchment have undergone drastic (CNR), Italy changes, including a volume increase of Lake Palcacocha between around 1990 and *Correspondence: 2010 by a factor of 34. In parallel, the population of Huaraz grew exponentially to more Holger Frey [email protected] than 120,000 inhabitants nowadays, making a comprehensive assessment and mapping of GLOF hazards for the Quillcay catchment and the city of Huaraz indispensable. -
476 the AMERICAN ALPINE JOURNAL Glaciers That Our Access Was Finally Made Through the Mountain Rampart
476 THE AMERICAN ALPINE JOURNAL glaciers that our access was finally made through the mountain rampart. One group operated there and climbed some of the high-grade towers by stylish and demanding routes, while the other group climbed from a hid- den loch, ringed by attractive peaks, north of the valley and intermingled with the mountains visited by the 1971 St. Andrews expedition (A.A.J., 1972. 18: 1, p. 156). At the halfway stage we regrouped for new objec- tives in the side valleys close to Base Camp, while for the final efforts we placed another party by canoe amongst the most easterly of the smooth and sheer pinnacles of the “Land of the Towers,” while another canoe party voyaged east to climb on the islands of Pamiagdluk and Quvernit. Weather conditions were excellent throughout the summer: most climbs were done on windless and sunny days and bivouacs were seldom contem- plated by the parties abseiling down in the night gloom. Two mountains may illustrate the nature of the routes: Angiartarfik (1845 meters or 6053 feet; Grade III), a complex massive peak above Base Camp, was ascended by front-pointing in crampons up 2300 feet of frozen high-angled snow and then descended on the same slope in soft thawing slush: this, the easiest route on the peak, became impracticable by mid-July when the snow melted off to expose a crevassed slope of green ice; Twin Pillars of Pamiagdluk (1373 meters or 4505 feet; Grade V), a welded pair of abrupt pinnacles comprising the highest peak on this island, was climbed in a three-day sortie by traversing on to its steep slabby east wall and following a thin 300-metre line to the summit crest. -
Folleto Inglés (1.995Mb)
Impressive trails Trekking in Áncash Trekking trails in Santa Cruz © J. Vallejo / PROMPERÚ Trekking trails in Áncash Áncash Capital: Huaraz Temperature Max.: 27 ºC Min.: 7 ºC Highest elevation Max.: 3090 meters Three ideal trekking trails: 1. HUAYHUASH MOUNTAIN RANGE RESERVED AREA Circuit: The Huayhuash Mountain Range 2. HUASCARÁN NATIONAL PARK SOUTH AND HUARAZ Circuit: Olleros-Chavín Circuit: Day treks from Huaraz Circuit: Quillcayhuanca-Cójup 3. HUASCARÁN NATIONAL PARK NORTH Circuit: Llanganuco-Santa Cruz Circuit: Los Cedros-Alpamayo HUAYHUASH MOUNTAIN RANGE RESERVED AREA Circuit: Huayhuash Mountain Range (2-12 days) 45 km from Chiquián to Llámac to the start of the trek (1 hr. 45 min. by car). This trail is regarded one of the most spectacular in the world. It is very popular among mountaineering enthusiasts, since six of its many summits exceed 6000 meters in elevation. Mount Yerupajá (6634 meters) is one such example: it is the country’s second highest peak. Several trails which vary in length between 45 and 180 kilometers are available, with hiking times from as few as two days to as many as twelve. The options include: • Circle the mountain range: (Llámac-Pocpa-Queropalca Quishuarcancha-Túpac Amaru-Uramaza-Huayllapa-Pacllón): 180 km (10-12 days). • Llámac-Jahuacocha: 28 km (2-3 days). Most hikers begin in Llámac or Matacancha. Diverse landscapes of singular beauty are clearly visible along the treks: dozens of rivers; a great variety of flora and fauna; turquoise colored lagoons, such as Jahuacocha, Mitucocha, Carhuacocha, and Viconga, and; the spectacular snow caps of Rondoy (5870 m), Jirishanca (6094 m), Siulá (6344 m), and Diablo Mudo (5223 m). -
Rutas Imponentes Rutas De Trekking En Áncash Ruta De Trekking Santa Cruz © J
Rutas imponentes Rutas de trekking en Áncash de Santa Cruz © J. Vallejo / PROMPERÚ trekking Ruta de Rutas de trekking en Áncash Áncash Capital: Huaraz Temperatura Máx.: 27 ºC Mín.: 7 ºC Altitud Máx.: 3090 msnm Tres rutas ideales para la práctica de trekking: 1. ZONA RESERVADA CORDILLERA HUAYHUASH (ZRCH) Circuito: Cordillera Huayhuash 2. PARQUE NACIONAL HUASCARÁN (PNH) SUR Y HUARAZ Circuito: Olleros-Chavín Circuito: Trekkings de 1 día desde Huaraz Circuito: Quillcayhuanca-Cójup 3. PARQUE NACIONAL HUASCARÁN (PNH) NORTE Circuito: Llanganuco-Santa Cruz Circuito: Los Cedros-Alpamayo ZONA RESERVADA CORDILLERA HUAYHUASH (ZRCH) Circuito: Cordillera Huayhuash (2-12 días) A 45 km de Chiquián a Llámac, donde se inicia la caminata (1 h 45 min en auto). Esta ruta es considerada como uno de los 10 circuitos más espectaculares en el mundo para el trekking. Además, es muy popular entre los aficionados al andinismo, pues entre sus múltiples cumbres, seis superan los 6000 m.s.n.m. Tal es el caso del nevado Yerupajá (6634 m.s.n.m.), el segundo más alto del país. Se pueden realizar diversas rutas que demandan entre 2 a 12 días de camino, por lo que la longitud del trekking varía según el tiempo de recorrido, siendo los promedios entre 45 y 180 kilómetros, así tenemos: • Rodear la cordillera (Llámac-Pocpa-Queropalca Quishuarcancha-Túpac Amaru-Uramaza-Huayllapa- Pacllón): 180 km (10-12 días). • Llámac-Jahuacocha: 28 km (2-3 días). La mayoría de caminantes suelen iniciar el recorrido en Llámac o Matacancha. Durante el recorrido es posible apreciar diversos paisajes de singular belleza como los espectaculares nevados: Rondoy (5870 m), Jirishanca (6094 m), Siulá (6344 m), Diablo Mudo (5223 m), entre otros; decenas de ríos; lagunas color turquesa como Jahuacocha, Mitucocha, Carhuacocha y Viconga; una gran diversidad de flora y fauna. -
ABSTRACTS Abstracts ~
INSTITUTE of ANDEAN STUDIES ~ABSTRACTS Abstracts ~ 57th Annual Meeting JANUARY 6–7, 2017 BERKELEY, CALIFORNIA 2 Friday, January 6h RANDALL HAAS , University of Wyoming; JAMES WATSON , University of Arizona Dental evidence for tuber intensification in the Titicaca Basin, 7kya Recent DNA studies point to the South Central Andes as a likely center of potato domestication. We present independent support for this hypothesis with new observations on dental-wear patterns among a burial population of 7000-year-old foragers discovered at the site of Soro Mik’aya Patjxa, Lake Titicaca Basin. Five of sixteen individuals exhibit lingual surface attrition of the maxillary anterior teeth. This observation along with other dental observations, contextual material evidence, and ethnographic comparisons converge to suggest that the Middle Archaic Period foragers of Soro Mik’aya habitually engaged in intensive tuber processing. New questions and implications for Andean domestication are discussed. MARIA BRUNO , Dickinson College; CHRISTINE A. HASTORF , University of California, Berkeley; AMANDA SANTILLI , JAMES CIARROCCA , Dickinson College; JEWELL SORIANO , University of California, Berkeley; JOSÉ CAPRILES FLORES , Pennsylvania State University Palimpsests of Chiripa landscape management The most prominent Andean political and ceremonial centers were not isolated architectural complexes but places made more potent by being situated within meaningful and managed socio ‐natural landscapes. Fine ‐scale topographic mapping around the monumental center of Chiripa, Bolivia by the Taraco Archaeological Project sheds new light onto a palimpsest of long ‐term landscape management of the area. Here, we begin to unpack this complex landscape by examining modified hydraulic features including springs, streams, and raised ‐fields. While this is a first step towards a better understanding of pre ‐ Hispanic management practices, it also reveals significant modifications associated with historic and present ‐day Chiripa communities. -
DAV Summit Club
Vorbereitungskurse / Trainingsexpedition / leichte Expeditionen / 6000er & Hochtouren / Südamerika / Peru TRAININGSEXPEDITION CORDILLERA BLANCA MIT NEVADO URUS, 5495 M, NEVADO ISHINCA, 5530 M UND NEVADO TOCLLARAJU, 6034 M Beschreibung Trainingsexpedition, einfach, 16 Tage Expeditionsbergsteigen kompakt lernen Drei Ziele unterschiedlicher Schwierigkeit: Nevado Urus 5495 m, Nevado Ishinca 5530 m, und auf den Anden-6000er Nevado Tocllaraju, 6034 m Tipps und Tricks von einem erfahrenen Expeditionsleiter Expeditionserfahrener, Deutsch sprechender einheimsicher Staatlich geprüfter Berg- und Skiführer Programm Schneebedeckte Eisriesen, blauer Himmel, gute Erreichbarkeit – das ist Expeditionsbergsteigen in Peru. Diese Trainingsexpedition mit drei attraktiven Gipfelzielen unterschiedlicher Schwierigkeit ist eine Mischung aus Ausbildungskurs und richtiger Expedition. „Learning by doing“ heißt hier die Devise. Für das Bergsteigen in großer Höhe erlernen Sie wichtige theoretische und praktische Inhalte, wie z. B. das Begehen von Fixseilen und die richtige Akklimatisationstechnik. Sie üben Bekanntes, wie die richtige Handhabung von Pickel und Steigeisen sowie Spaltenbergung intensiv ein. Anschließend haben Sie ausreichend Gelegenheit, das Ganze auf einer richtigen Expedition anzuwenden. Ziel der Veranstaltung ist es, den routinierten Hochtourengeher systematisch auf die Teilnahme an einer größeren Expedition vorzubereiten. Erläuterungen: Gz 5 h Die Gehzeit ohne Pausen beträgt fünf Stunden. [F/M/–] [F/–/A] [–/–/A] Enthaltene Mahlzeiten: F = Frühstück; M = Mittagessen; A = Abendessen. 1. Tag: Abflug Flug mit Air Europa von Frankfurt über Madrid. 2. Tag: Huaraz, 3100 m Nach der frühmorgendlichen Ankunft in Lima fahren wir nach Huaraz über den 4100 m hohen Conacocha-Pass. Mittagessen in Barrancas, wo Sie von der Panamericana in Richtung der Weißen Kordilliere abzweigen. Hotelübernachtung. Fz ca. 8 h [-/M/A] 3. Tag: Huaraz, 3100 m Tag zur freien Verfügung, der für die Höhenanpassung vorgesehen ist. -
Glacial Flooding and Disaster Risk Management Knowledge Exchange and Field Training
GLACIAL FLOODING AND DISASTER RISK MANAGEMENT KNOWLEDGE EXCHANGE AND FIELD TRAINING July 11-24, 2013 Huaraz, Peru July 16, 2013 Day 4 - Field Methods and Modules I Glacial lakes and emerging risks in the Cordillera Blanca Wilfred Haeberli, Marcelo Somos-Valenzuela and Cesar Portocarrero 1. Introduction Continued atmospheric warming induces striking changes of most glaciers around the world (WGMS 2008). The formation of new lakes in de-glaciating high-mountain regions (Linsbauer et al., 2012) strongly influences landscape characteristics and represents a significant hazard related to climate change (Haeberli et al. , 2010; Kattelmann 2003; Richardson and Reynolds 2000). An increasing number of numerical modeling studies indicate that mountain glaciers are likely to continue vanishing (Zemp et al. 2006); that a fifth of Canada's Arctic Archipelago glaciers may disappear by the end of the century (Lenearts et al. 2013); that up to 50 percent of the Andes glaciers may have already been lost to climate-induced melting (Rabatel et al. 2013); and that Himalayan glaciers are reported to be losing mass as well, although with notable exceptions in the Karakoram and Northwestern Himalaya (Bolch et al. 2012). Major effects of this trend in glacier recession are increased variability in water supplies in some regions (Huss, 2011) and flooding risks from lakes formed at receding glaciers (Clague and Evans, 2000; Haeberli et al., 2010). The goals of this module and visit to Laguna Llaca are to (a) Understand the formation, characteristics and further evolution of new lakes due to glacier retreat in the Cordillera Blanca; (b) exchange knowledge end experience regarding the assessment of potential hazards due to glacier floods and debris flows; (c) discuss corresponding possibilities of hazard prevention and safety systems; and (d) consider consequences of glacier retreat to fresh-water supply and related adaptation strategies. -
Geografía Y Medio Ambiente
ALMANAQUE DE ANCASH 2002-2003 103 GEOGRAFIA Y MEDIO AMBIENTE Silhueta del Mapa del Perú encima de la Laguna de Querococha (Recuay) II. GEOGRAFIA Y MEDIO AMBIENTE EN EL PERU EN EL MUNDO 104 ALMANAQUE DE ANCASH 2002-2003 SUMARIO GEOGRAFIA Y MEDIO AMBIENTE EN EL PERU EN EL MUNDO ALMANAQUE DE ANCASH 2002-2003 105 SUMARIO Página 2.1 Características geográficas ................................................................................................................................. 107 2.1.1 Superficie Territorial ................................................................................................................................. 107 2.1.1.1 Ancash: Superficie insular: 2002 .............................................................................................................. 107 2.1.1.2 Ancash: superficie, población total proyectada y desidad poblacional, según provincias: 2001- 2002 107 a) Mapa del Perú: Ubicación Geográfica del Departamento de Ancash ...................................................... 108 2.1.2 Ubicación geográfica .................................................................................................................................. 109 2.1.3 Clima y Temperatura ................................................................................................................................ 110 2.1.4 Hidrografía ................................................................................................................................................. 111 a) Vertiente de Pacífico................................................................................................................................. -
USAID Glacial Lake Handbook 2014
TECHNICAL REPORT THE GLACIAL LAKE HANDBOOK REDUCING RISK FROM DANGEROUS GLACIAL LAKES IN THE CORDILLERA BLANCA, PERU February 2014 This publication is made possible by the support of the American people through the United States Agency for International Development (USAID). It was prepared by Engility Corporation and the High Mountains Adaptation Partnership. ! This report has been prepared for the United States Agency for International Development (USAID), under the Climate Change Resilient Development Task Order No. AID-OAA-TO-11- 00040, under The Integrated Water and Coastal Resources Management Indefinite Quantity Contract (WATER IQC II) Contract No. AID-EPP-I-00-04-00024. Engility Corporation Contact: Glen Anderson, Chief of Party, [email protected] Engility Corporation 1211 Connecticut Ave., NW Suite 700 Washington, DC 20036 Cover Photo: César A. Portocarrero Rodríguez, The Mountain Institute ! THE GLACIAL LAKE HANDBOOK REDUCING RISK FROM DANGEROUS GLACIAL LAKES IN THE CORDILLERA BLANCA, PERU February 2014 Prepared for: United States Agency for International Development Global Climate Change Office, Climate Change Resilient Development Project Washington, DC Prepared by: César A. Portocarrero Rodríguez The Mountain Institute Washington, DC and Engility Corporation Washington, DC Editorial assistance: Betsy Armstrong, Glen Anderson, Alton Byers, Jamie Carson, Michael Cote, John Harlin, Meghan Hartman, Daene McKinney, and Jonathan Schwarz Contact: Michael Cote, Engility Corporation, [email protected] DISCLAIMER -
Revista De Glaciares Y Ecosistemas De Montaña
ISSN 2519-7649 Revista de Glaciares y Ecosistemas de Montaña Año 2, Número 3 – Diciembre 2017 INAIGEM Instituto Nacional de Investigación en Glaciares y Ecosistemas de Montaña Huaraz, Ancash, Perú Revista de Glaciares y Ecosistemas de Montaña INAIGEM Presidente Ejecutivo Ing. Benjamín Morales Arnao Secretario General Sr. Jorge Rojas Fernández Editor Mg. Steven A. Wegner Comité Editorial Sr. Jorge Rojas Fernández Ing. Ricardo Villanueva Ramírez Dr. Roberto Arias Flores Comité Consultivo Dr. Lonnie Thompson (School of Earth Sciences, The Ohio State University, Columbus, EE.UU.) Dr. Cedomir Marangunic Damianovic (Geoestudios, Santiago, Chile) Dr. Bernard Francou (LTHE - Laboratoire d’étude des Transferts en Hidrologie et Environnement, Grenoble, Francia) Prof. Dr. Wilfried Haeberli (Geographisches Institut, Universität Zürich, Suiza) Ing. Zaniel Novoa Goicochea (Pontificia Universidad Católica del Perú, Lima) Dr. Jeffrey S. Kargel (Department of Hydrology & Atmospheric Sciences, The University of Arizona, Tucson, EE.UU.) Dr. Enrique Flores Mariazza (Laboratorio de Utilización de Pastizales, Universidad Nacional Agraria La Molina, Lima) Dr. Hildegardo Córdova Aguilar (Centro de Investigación en Geografía Aplicada, Pontificia Universidad Católica del Perú, Lima) Dr. Bryan G. Mark (Department of Geography, The Ohio State University, Columbus, EE.UU.) La Revista de Glaciares y Ecosistemas de Montaña es una publicación científica de periodicidad semestral (junio y diciembre). Tiene como objetivo difundir los resultados de trabajos de investigación en glaciares y ecosistemas de montaña desarrollados en los Andes, especialmente en el Perú, pero también en otros países andinos. La revista publica artículos científicos originales e inéditos especialmente en las áreas de glaciología y ecología de ecosistemas de montaña, así como disciplinas afines de ciencias de la tierra, ciencias biológicas y ciencias sociales. -
USAID Peru Local Adaptation Plan of Action LAPA
TECHNICAL REPORT QUILLCAY PLAN DE ACCION LOCAL PARA LA ADAPTACIÓN AL CAMBIO CLIMATICO SUBCUENCA DE QUILLCAY, MANCOMUNIDAD MUNICIPAL WARAQ DICIEMBRE 2014 This publication is made possible by the support of the American people through the United States Agency for International Development (USAID). It was prepared by Engility Corporation and University of Austin- Texas. This report has been prepared for the United States Agency for International Development (USAID), under the Climate Change Resilient Development Task Order No. AID-OAA-TO-11- 00040, under The Integrated Water and Coastal Resources Management Indefinite Quantity Contract (WATER IQC II) Contract No. AID-EPP-I-00-04-00024. Engility Corporation Contact: Glen Anderson, Chief of Party, [email protected] Engility Corporation 1320 Braddock Place Alexandria, VA 22314 Cover Photo: University of Austin-Texas 1. Introducción 4 1.1. De un proyecto de reducción del riesgo de avalanchas en lagos glaciares a la gestión integrada de cuencas 4 1.2. Una alianza estratégica 6 1.3. Proceso de la “Mesa de Trabajo Palcacocha” 7 2. Antecedentes 10 2.1 Relación con la política regional y nacional de adaptación 10 2.2 Objetivos y principios generales del proceso 13 2.3 Descripción general del proceso de 7 pasos 14 3. Peligros climáticos y no climáticos en la subcuenca de Quillcay 16 3.1 Características físicas, riesgos y vulnerabilidades 16 3.2 Características socioeconómicas, riesgos y vulnerabilidades 25 3.3 Capacidad institucional para abordar los riesgos y vulnerabilidades 35 4. Quillcay: Proceso de Consulta para el Plan de Adaptación Local en las zonas rural y urbana. 46 4.1 Paso 1.