DOCSLIB.ORG

Los Represamientos Hidráulicos Prehispánicos En El Flanco Occidental De La Cordillera Negra, Áncash, Perú

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Los Represamientos Hidráulicos Prehispánicos En El Flanco Occidental De La Cordillera Negra, Áncash, Perú Volumen 52, N° 4, 2020. Páginas 541-560 Chungara Revista de Antropología Chilena LOS REPRESAMIENTOS HIDRÁULICOS PREHISPÁNICOS EN EL FLANCO OCCIDENTAL DE LA CORDILLERA NEGRA, ÁNCASH, PERÚ PREHISPANIC HYDRAULIC DAMMING ON THE WESTERN SIDE OF THE CORDILLERA NEGRA, ANCASH, PERÚ Jesús Maza1,2 y Andy Combey2,3 Este articulo presenta el estudio de las estructuras hidráulicas conocidas como represas, ubicadas en la subcuenca del Río Jimbe en la cabecera del Valle de Nepeña (Áncash), a partir de prospecciones sistemáticas en el área referida. La investigación permitió registrar 14 represamientos prehispánicos dentro de tres distintas quebradas. El análisis morfológico y espacial de estos sistemas hidráulicos sugiere un manejo diferenciado del agua en el flanco occidental de la Cordillera Negra y aboga por una reevaluación de las estrategias de explotación del territorio por los grupos serranos durante la época prehispánica tardía. Palabras claves: represas, Cordillera Negra, pastoralismo, riego, prehispánico. This article presents a study of the hydraulic structures -known as dams- in the Jimbe River sub-basin of the headwaters of the Nepeña Valley (Ancash), based on systematic surveys carried out in that sector. This study allowed for recording 14 pre-Hispanic dams in three different sub-valleys. The morphological and spatial analysis of these hydraulic systems suggests differentiated management of water on the western side of the Cordillera Negra and provides evidence for a reassessment of land use strategies set up by Sierra people during the late pre-Hispanic Period. Key words: Dams, Cordillera Negra, pastoralism, irrigation, pre-Hispanic. El manejo del agua se constituye como un tema central en el ámbito geográfico (Pulgar Vidal 1998), podrían para el entendimiento de la organización socioeconómica reflejar las estrategias de subsistencia de las sociedades de los grupos humanos que habitaron el paisaje andino que las construyeron y que, en consecuencia, se (Carrión Cachot 2005 [1955]; Consejo Andino 1988; vieron beneficiados por el funcionamiento de estas Gelles 2002; Gerbrandy y Hoogendam 1998; Kosok obras hidráulicas. Uno de los temas abordados aun 1965). Los grupos humanos prehispánicos asentados incipientemente desde el punto de vista arqueológico es en las estribaciones occidentales de los Andes se el referido a las estructuras hidráulicas conocidas como desarrollaron en medios naturales que solían carecer de represas. recursos hídricos estables. En ese sentido, el extenso sistema hidráulico Huiru La Cordillera Negra, sistema orográfico regional Catac1, ubicado en el valle alto de Jimbe (Maza 2018b, que corre paralelo a la costa ancashina a una distancia 2018c), y sus numerosas lagunas represadas (Combey promedio de 60 km, sin glaciares y fuentes de agua 2018b; Gambini 1975; Llosa 2008) en épocas pasadas, permanente, representa una región natural peculiar, que destacan por su cantidad de inversión hidráulica y permite conocer los desafíos que deben enfrentar las brindan un escenario interesante para evaluar el papel poblaciones en ecosistemas de altura. Para proveerse de estas tecnologías en el mundo andino prehispánico. eficientemente del agua, las sociedades locales desarrollaron La presente investigación presenta, de manera varios mecanismos. preliminar los resultados de las investigaciones en la La evidencia encontrada en las distintas fuentes parte septentrional del valle alto de Nepeña, e intenta sugiere que las represas hidráulicas, conocidas como aproximarse a la comprensión de estas estructuras qochas en el mundo andino (Vivanco 2015), o lagunas hidráulicas. 1 Universidad Nacional Mayor de San Marcos, Lima, Perú. [email protected] 2 Círculo Cultural Cordillera Negra, Lima, Perú. 3 Université Grenoble Alpes, CNRS (Centre National de la Recherche Scientifique), IRD (Institut de Recherche pour le Développement), IFSTTAR (Institut français des sciences et technologies des transports, de l’aménagement et des réseaux), ISTerre (Institut des Sciences de la Terre), Grenoble, France. [email protected] Recibido: octubre 2018. Aceptado: diciembre 2019. 542 Jesús Maza y Andy Combey Características Geográficas y Medioambientales Geológicamente, la zona de estudio está compuesta por formaciones terciarias de Calipuy La zona de investigación comprende las partes altas volcánico alternadas con sustratos geológicos del del distrito de Cáceres del Perú (provincia de Santa, Cretácico (formaciones Santa-Carhuaz), así como Áncash), en el flanco occidental de la sección norte de un gran componente de granodiorita tonalita para el la Cordillera Negra. Las características principales de área superior de la Quebrada Capado especialmente2. este medio natural corresponden a las descripciones Esas rocas, puntualmente fracturadas como los generales otorgadas para la región Suni y Puna de la depósitos fluvio-glaciares ubicados en los fondos de región andina (Pulgar Vidal 1998), aunque también las quebradas, constituyen acuíferos de “productividad comparte características que corresponden a la puna de elevada” (Sistema de Información Geográfica del los Andes centrales (Custred 1977). GEOCATMIN)3. La cuenca del Río Jimbe se origina por la En el marco de esta investigación se han confluencia de los numerosos cursos de agua que prospectado las cabeceras de tres quebradas principales descienden del flanco occidental de la Cordillera Negra, (nombradas de norte a sur): Capado, Huampucayán y generalmente siguiendo una orientación suroeste. Mátar. Si bien las tres quebradas comparten similares Las quebradas de mayor importancia se caracterizan características geográficas y medioambientales por por tener cursos de agua que se originan usualmente ubicarse en zonas ecológicas comparables, existen en las lagunas situadas en sus cabeceras. Muchas de algunas diferencias que debemos tener en cuenta y que estas lagunas naturales se encuentran actualmente señalaremos a continuación. represadas con materiales modernos, aunque las bases o La primera, la Quebrada Capado, se encuentra en la cimientos de las mismas correspondan posiblemente a parte nororiental del distrito y contiene en sus cabeceras represamientos prehispánicos, posiblemente tardíos. abundantes zonas planas que podrían representar Según Gambini (1975), el Río Jimbe nace de la probables zonas de pastoreo en la antigüedad4 y que Laguna Huampucayán y sigue su curso río abajo para podrían denominarse pequeñas mesetas. Asimismo, no unirse con otras quebradas y riachuelos. Los de mayor se encuentran núcleos poblaciones en sus proximidades, importancia lo componen los tributarios que bajan de salvo algunas unidades habitacionales temporales las quebradas (de norte a sur) de Lampanín, Capado, (chozas) de pastores provenientes del caserío moderno Huirí, Huampucayán, Mátar y Cosma (Figura 1). de Carhuamarca. Según versiones locales, la cabecera Figura 1. Valle alto de Jimbe y distribución de los sitios presentados. Créditos Andy Combey. High Jimbe Valley and layout of sites in the article. Credit: Andy Combey. Los represamientos hidráulicos prehispánicos en el flanco occidental de la Cordillera Negra, Áncash, Perú 543 de esta quebrada ha sido motivo de controversia y Ancoracá, ubicado en el flanco oriental de la Cordillera disputa con las comunidades de Huaylas y Santo Toribio Negra, siguiendo un sendero ubicado en el sector sur hasta hace algunos años. La raíz del conflicto ha sido del complejo de lagunas. Este camino parece ser de esencialmente el control de los pastos y los recursos considerable antigüedad y podría corresponder a la naturales del área. Las lagunas situadas en las cabeceras vía que refería Raimondi comentada líneas arriba. de esta quebrada suelen ser visitadas por los pobladores Actualmente, los pobladores de Peras y Mucharán de los caseríos de ambos flancos de la Cordillera Negra representan los principales visitantes de estas alturas, por contener fauna lacustre. Debemos agregar que aunque se percibe una mayor posesión del pueblo de también se visitó un afluente de la quebrada Capado Peras, posiblemente debido a su cercanía. No obstante, por su margen derecha, conocida como la quebrada las labores de refacción realizadas a los diques de Ulto Cruz. En la cabecera de este pequeño tributario es las lagunas provienen de ambos lados. Existe un posible encontrar un número considerable de cabezas marcado contraste geográfico si consideramos la zona de ganado vacuno de pastores de los pueblos de Rayán ubicada arriba de la Laguna Quepancocha y la situada y Racuaybamba. en su parte inferior. Mientras que la primera presenta La segunda, la Quebrada Huampucayán, es principalmente una superficie rocosa con muy poca mencionada ya en el siglo XIX (Figura 2) por Raimondi5 vegetación, la parte inferior a esta laguna contiene (1873:111), quien señala que por ella traficaban los mayor cantidad de pastos, principalmente ichu (Stipa comerciantes de Huaylas que se dirigían a la costa6. La ichu). cabecera de esta quebrada está interconectada por una Finalmente, la cabecera de la Quebrada Mátar, serie de lagunas que, vistas desde imágenes satelitales, presenta la cuenca más estrecha de las quebradas conforman un conjunto de lagunas que encierran una identificadas. Esencialmente, posee una forma de “V” forma circular en un radio no superior a los 1,5 km. que aumenta mientras va descendiendo en sus partes La superficie de esta cabecera está caracterizada por medias y bajas. Contiene el mayor espejo de agua poseer una aridez extrema y generalmente rocosa. identificado, la Laguna Mamancocha,
Load more

Recommended publications
  • Hydrochemical Evaluation of Changing Glacier Meltwater Contribution To
    (b) Rio Santa U53A-0703 4000 Callejon de Huaylas Contour interval = 1000 m 3000 0S° Hydrochemical evaluation of changing glacier meltwater 2000 Lake Watershed Huallanca PERU 850'° 4000 Glacierized Cordillera Blanca ° Colcas Trujillo 6259 contribution to stream discharge, Callejon de Huaylas, Perú 78 00' 8S° Negra Low Cordillera Blanca Paron Chimbote SANTA LOW Llullan (a) 6395 Kinzl ° Lima 123 (c) Llanganuco 77 20' Lake Titicaca Bryan G. Mark , Jeffrey M. McKenzie and Kathy A. Welch Ranrahirca 6768 910'° Cordillera Negra 16° S 5000 La Paz 1 >4000 m in elevation 4000 Buin Department of Geography, The Ohio State University, Columbus, OH 43210, USA,[email protected] ; 6125 80° W 72° W 3000 2 Marcara 5237 Department of Earth Sciences, Syracuse University, Syracuse New York, 13244, USA,[email protected] ; Anta 5000 Glaciar Paltay Yanamarey 3 JANGAS 6162 4800 Byrd Polar Research Center, The Ohio State University, Columbus, OH 43210, USA, [email protected] YAN Quilcay 5322 5197 Huaraz 6395 4400 Q2 4800 SANTA2 (d) 4400 Olleros watershed divide4400 ° Q1 Q3 4000 ABSTRACT 77 00' Querococha Yanayacu 950'° 3980 2 Q3 The Callejon de Huaylas, Perú, is a well-populated 5000 km watershed of the upper Rio Santa river draining the glacierized Cordillera 4000 Pachacoto Lake Glacierized area Blanca. This tropical intermontane region features rich agricultural diversity and valuable natural resources, but currently receding glaciers Contour interval = 200 m 2 0 2 4km are causing concerns for future water supply. A major question concerns the relative contribution of glacier meltwater to the regional stream SETTING The Andean Cordillera Blanca of Perú is the most glacierized mountain range in the tropics.
    [Show full text]
  • X-Ray Fluorescence Analysis of Ceramics from Santa Rita B, Northern Peru Pamela Shwartz
    Florida State University Libraries Electronic Theses, Treatises and Dissertations The Graduate School 2010 X-Ray Fluorescence Analysis of Ceramics from Santa Rita B, Northern Peru Pamela Shwartz Follow this and additional works at the FSU Digital Library. For more information, please contact [email protected] THE FLORIDA STATE UNIVERSITY COLLEGE OF ARTS AND SCIENCES X-RAY FLUORESCENCE ANALYSIS OF CERAMICS FROM SANTA RITA B, NORTHERN PERU By PAMELA SHWARTZ A Thesis submitted to the Department of Anthropology in partial fulfillment of the requirements for the degree of Master of Science Degree Awarded: Spring Semester, 2010 The members of the committee approve the thesis of Pamela Shwartz defended on October 13, 2008. __________________________________ Cheryl Ward Professor Co-Directing Thesis __________________________________ Glen Doran Professor Co-Directing Thesis __________________________________ Mary Pohl Committee Member __________________________________ Michael Uzendoski Committee Member __________________________________ Jonathan Kent Committee Member Approved: _____________________________________ Glen Doran, Chair, Anthropology _____________________________________ Joseph Travis, Dean, College of Arts and Sciences The Graduate School has verified and approved the above-named committee members ii ACKNOWLEDGMENTS I would like to acknowledge the many people who have given me the time, energy, and support to finish this thesis. First of all I would like to thank Jonathan Kent for the opportunity to work on the PASAR project at Santa Rita B in 2006 and 2007. It was a wonderful experience. I am grateful to Professor Jonathan Kent, Victor Vásquez Sanchez, and Theresa Rosales Tham for the many explanations of Andean archaeology and the enthusiasm they imparted to me for North Coast Peruvian archaeology. I would like to further thank Victor and Theresa for their friendship, endless information, and their patience with my imperfect Spanish.
    [Show full text]
  • New Geographies of Water and Climate Change in Peru: Coupled Natural and Social Transformations in the Santa River Watershed
    New Geographies of Water and Climate Change in Peru: Coupled Natural and Social Transformations in the Santa River Watershed Jeffrey Bury,∗ Bryan G. Mark,† Mark Carey,‡ Kenneth R. Young,§ Jeffrey M. McKenzie,# Michel Baraer,¶ Adam French,∗ and Molly H. Polk§ ∗Department of Environmental Studies, University of California, Santa Cruz †Department of Geography and Byrd Polar Center, The Ohio State University ‡Robert D. Clark Honors College, University of Oregon §Department of Geography and the Environment, University of Texas, Austin #Earth and Planetary Sciences, McGill University ¶Ecole´ de technologie superieure,´ UniversiteduQu´ ebec´ Projections of future water shortages in the world’s glaciated mountain ranges have grown increasingly dire. Although water modeling research has begun to examine changing environmental parameters, the inclusion of social scenarios has been very limited. Yet human water use and demand are vital for long-term adaptation, risk reduction, and resource allocation. Concerns about future water supplies are particularly pronounced on Peru’s arid Pacific slope, where upstream glacier recession has been accompanied by rapid and water-intensive economic development. Models predict water shortages decades into the future, but conflicts have already arisen in Peru’s Santa River watershed due to either real or perceived shortages. Modeled thresholds do not align well with historical realities and therefore suggest that a broader analysis of the combined natural and social drivers of change is needed to more effectively understand the hydrologic transformation taking place across the watershed. This article situates these new geographies of water and climate change in Peru within current global change research discussions to demonstrate how future coupled research models can inform broader scale questions of hydrologic change and water security across watersheds and regions.
    [Show full text]
  • Recent Progress in Understanding the Hydro-Climate System of the Andes: Physical Processes and Resources for Andean Populations
    Recent progress in understanding the hydro-climate system of the Andes: Physical processes and resources for Andean populations Chat, Tuesday, 05 May, 14h – 15h45 14h. Introduction: Jhan Carlo Espinoza, Wouter Buytaert, Katja Trachte and Germán Poveda Sub-session 1: Climatology and atmospheric sciences Chair: K. Trachte and JC. Espinoza. 14:05 Block 1 1. (Invited) The GEWEX High Mountain Activities and Its Relevance to the Andean Region - Peter van Oevelen 14:10 Block 2 2. Environmental change effects on canopy water fluxes of a tropical mountain rain forest in the Andes of Ecuador - Jörg Bendix 3. Observed local drivers of rainfall variability and changes in the Rio Santa Basin, Tropical Andes of Peru - Cornelia Klein(ECS) 4. Laboratory of Atmospheric Microphysics and Radiation (LAMAR): a set of sensors for the study of extreme meteorological events in the Central Andes of Peru - Daniel Martinez 14:20 Block 3 5. Atmospheric physics and microphysics research project in the Central Peruvian Andes. A multilateral approach - Yamina Silva 6. Spatio-temporal temperature and precipitation patterns in the southern Peruvian Andes - insights from the Climandes project - Christoph Spirig 7. Long-term variability of central Andes precipitation in the IPSL- CM6A-LR model: origin and causes - Julián Villamayor(ECS) 14:30 Block 4 8. The annual and diurnal cycles of precipitation over an Equatorial Andean valley and its transition to the Amazon Basin: A case at the Antizana region – Jean Carlos Ruiz 9. Precipitation diurnal cycle and associated valley wind circulations over an Andean glacier region (Antizana, Ecuador) – Clémentine Junquas 10. The coastal El Niño-Event of 2017 in Ecuador and Peru - a weather Radar analysis - Rütger Rollenbeck 11.
    [Show full text]
  • The Callejon and the Santa
    NOT FOR PUBLICATION INSTITUTE OF CUKKENT WOKLD AFFAIKS WH l Uphill Farm The Callej6n and the Santa Conway, assachusets July 23, 1956 r. Walter S. Rogers Institute of Current World Affairs 522 Fifth Avenue New York 6, New York Dear r. Rogers- The old woman had been dead five days. She had been poor durin he life so poor that no one had killed a cow to honor her in death. There was no money to pay for luxuries like fresh bef or perhaps a wooden coffin. The old woman had few relatives living on the hacienda who could afford anything more than the alcohol for the bearers and chanters. Therefore, when they carried her to the cemetery the old woman was swathed in a rough shroud and lashed to a pole stretcher. What is more, she had be- gun to smell a little by that time. Even in the altitude five days is a long time for the dead to remain above ground. Thee was no priest at the hacienda chapel; in the moun- tains there are too many chapels and very few priests. The chapel doors were closed to the old woman and her party, but the bearers brought her to the portal and placed her on the stones. The chanter screwed up his face an buged +/-s eyes at he uechua translation f the Catholic burial service pinted on the filthy pages of his book. It was necessary that he should do this in order to show the handful of spectstors_the concentrstion and the physical effort involved iu eding.
    [Show full text]
  • In Search of the Great Wall of Peru
    IN SEARCH OF THE GREAT WALL OF PERU Donald A. Proulx Professor of Anthropology, Emeritus University of Massachusetts Introduction and Summary of the Expedition In 1934, while undergraduate students at Yale and Harvard Universities respectively, Richard James Cross (1915-2003) and his friend Cornelius Van Schaak Roosevelt, (1915-1991) made a trip together to Peru. Their junket seems to have been motivated by Roosevelt’s reading an article about the Shippee-Johnson Peruvian Expedition of 1931 during which an ancient stone wall was discovered in the Santa Valley while taking aerial photographs of the Peruvian coast (Shippee 1932). Once in Peru Roosevelt and Cross contacted the eminent Peruvian archaeologist Julio C. Tello, who was planning a trip to the north coast and the Callejon de Huaylas in the mountains (Fig. 1). He generously invited the two young men to accompany him as his photographers. The team traveled from Lima up the coast stopping first at Huacho [in the Huaura Valley] and on to Paramonga, Fortaleza, and then Huarmay where they photographed a newly excavated ancient drum. Stopping in the Casma valley, they visited the ruins of Chanquillo (which Tello had visited but not photographed) and the adjacent 13 structures. It appears that they may also have photographed the Chimú administrative center of Manchan (see Roosevelt 1935: Fig. 6). They continued on to the Santa Valley where they investigated the “great wall” and traced its beginnings near to the coast. In Santa they also investigated several cemeteries, an ancient irrigation system and various ruins including a “fortress.” After spending several days in the Santa Valley, they took the train from Chimbote up the Santa Valley to its terminus at Huallanca and then by truck to Caraz where they photographed some monoliths in 1 private collections.
    [Show full text]
  • New Geographies of Water and Climate Change in Peru: Coupled Natural and Social Transformations in the Santa River Watershed
    New Geographies of Water and Climate Change in Peru: Coupled Natural and Social Transformations in the Santa River Watershed Jeffrey Bury,∗ Bryan G. Mark,† Mark Carey,‡ Kenneth R. Young,§ Jeffrey M. McKenzie,# Michel Baraer,¶ Adam French,∗ and Molly H. Polk§ ∗Department of Environmental Studies, University of California, Santa Cruz †Department of Geography and Byrd Polar Center, The Ohio State University ‡Robert D. Clark Honors College, University of Oregon §Department of Geography and the Environment, University of Texas, Austin #Earth and Planetary Sciences, McGill University ¶Ecole´ de technologie superieure,´ UniversiteduQu´ ebec´ Projections of future water shortages in the world’s glaciated mountain ranges have grown increasingly dire. Although water modeling research has begun to examine changing environmental parameters, the inclusion of social scenarios has been very limited. Yet human water use and demand are vital for long-term adaptation, risk reduction, and resource allocation. Concerns about future water supplies are particularly pronounced on Peru’s arid Pacific slope, where upstream glacier recession has been accompanied by rapid and water-intensive economic development. Models predict water shortages decades into the future, but conflicts have already arisen in Peru’s Santa River watershed due to either real or perceived shortages. Modeled thresholds do not align well with historical realities and therefore suggest that a broader analysis of the combined natural and social drivers of change is needed to more effectively understand the hydrologic transformation taking place across the watershed. This article situates these new geographies of water and climate change in Peru within current global change research discussions to demonstrate how future coupled research models can inform broader scale questions of hydrologic change and water security across watersheds and regions.
    [Show full text]
  • Follow the Water: Emerging Issues of Climate Change and Conflict in Peru
    Follow the Water: Emerging Issues of Climate Change and Conflict in Peru CMM Discussion Paper No. 5 June 2012 This publication was produced for review by the United States Agency for International Development. It was prepared by Jeffrey Stark, Sergio Guillén, and Cynthia Brady. ACKNOWLEDGEMENTS The field research team would like to acknowledge the important contributions of Claudia Rohrhirsch and Fernando Chávez of USAID/Peru, who coordinated the team’s meetings and provided valuable guidance and input during the study. The team also would like to extend its sincere thanks to Dr. Karen Kraft and her colleagues at AEDES, who provided gracious assistance and made key interviews possible in Arequipa Region, and to the TMI team in Huaraz. CREDITS: This report was written by Jeffrey Stark of the Foundation for Environmental Security and Sustainability (FESS) based on field research in Peru conducted by Jeffrey Stark, Sergio Guillén, FESS consultant, and Cynthia Brady, Senior Conflict Advisor, Office of Conflict Management and Mitigation, USAID. COVER PHOTO: FESS MOUNT HUASCARÁN, ANCASH REGION, PERU Follow the Water: Emerging Issues of Climate Change and Conflict in Peru CMM Discussion Paper No. 5 DISCLAIMER Discussion Papers have been commissioned by the Office of Conflict Management and Mitigation to initiate or advance consideration of important issues of conflict prevention or peacebuilding. As such they are not official documents. The author’s views expressed in this publication do not necessarily reflect the views of the United States
    [Show full text]
  • Giacial Lake Outburst Floods in the Area of Huaras, Cordillera Bianca, Peru
    STUI)lA GEOMORPHOLOCICA CARPATHO-BALCANICA VOL XXXIX KRAICÓW 2005 PL BSN 008lJ5434 L A N D F O R M E V O L U T I O N I N M O U N T A I N A R E A S ViT VILiMEKi (PRAHA), jAN KLIMEŚ9 (PRAm), MARCO L. ZAPATA3 (HUARAS) GIACIAL LAKE OUTBURST FLOODS IN THE AREA OF HUARAS, CORDILLERA BIANCA, PERU Abstract. mstorical records proved repeating occurrence and extremely high damaging potential of glacial lake outburst floods (GLOFs) - local name aluviones, which are caused by outbursts of large amoun( of wa(er from glacial ]akes in (he Cordil]era Blanca Moun(ains. Archive sources as wel] as in- [erpretation of SPOT and IANDSAT satellile images have been used lo describe past history of GLOF 's in the Cordillera Blanca Mountains. The origin and evolution or glacial lakes and recent conditions in- fluencing GLOFs hazard of selecled lakes have been evaluated in respect to ongoing climate warm- ing. Substantial enlargement of lakes surface areas were detected using ground measuremen[s and satellite imagery. Contemporary risk imposed by na(ural hazards connected with glacial lakes on the regional capilal city of Huarźs, has been evaluated. The research has proved thai ihe climate warming and deglaciation play signiricant role in the change of natural hazards conditions in high mountains. Kęy words: glacia] lakes, natural hazards, slope movements, flooding, Cordil]era Blanca, Peru INRODUCTION Mountain range of the Cordillera Blanca, which is part of the Western Cordil- lera (Cordillera Occidental) is situated in the northem Peru. Cordillera Occidental is in this part of Andes divided into two major mountain ranges trending from the NW to the SE.
    [Show full text]
  • Glacial Retreat and Adaptation Options in Peru's Rio Santa Basin
    ADAPTATION TO CLIMATE CHANGE: CASE STUDY – GLACIAL RETREAT AND ADAPTATION OPTIONS IN PERU’S RIO SANTA BASIN (DRAFT FINAL) January 2011 This report was produced for review by the United States Agency for International Development (USAID). It was prepared by International Resources Group (IRG). COVER PHOTO: Pastoruri Glacier, Cordillera Blanca, Peru ADAPTATION TO CLIMATE CHANGE: CASE STUDY – GLACIAL RETREAT AND ADAPTATION OPTIONS IN PERU’S RIO SANTA BASIN January 2011 DISCLAIMER This report was prepared by Daene C. McKinney, the University of Texas at Austin, Glen Anderson, International Resources Group, and Alton Byers, The Mountain Institute. The author’s views expressed in this publication do not necessarily reflect the views of the United States Agency for International Development or the United States Government TABLE OF CONTENTS 1. INTRODUCTION ············································································································ 1 1.1. Background .................................................................................................................................................... 1 1.1.1. Peru ..................................................................................................................................................................................... 1 1.1.2. Rio Santa Basin .............................................................................................................................................................. 1 1.2. Case Study Objectives ...............................................................................................................................
    [Show full text]
  • Implications of Geomorphological Research for Recent and Prehistoric Avalanches and Related Hazards at Huascaran, Peru
    Nat Hazards (2009) 50:193–209 DOI 10.1007/s11069-008-9330-7 ORIGINAL PAPER Implications of geomorphological research for recent and prehistoric avalanches and related hazards at Huascaran, Peru Jan Klimesˇ Æ Vı´t Vilı´mek Æ Marek Omelka Received: 11 June 2008 / Accepted: 24 November 2008 / Published online: 13 December 2008 Ó Springer Science+Business Media B.V. 2008 Abstract Detailed research of superficial deposits below the northern peak of Huascaran (Cordillera Blanca) provides new information on the limits of a paleo-avalanche origi- nating from this mountain. Geomorphological mapping of the sediments identified glacial deposits, deposits from historical rock-debris avalanches and huge boulders from a paleo- avalanche. Schmidt Hammer rock-hardness tests were used to distinguish between the several generations of rock-debris avalanches, but largely failed to distinguish between the much older moraine and the paleo-avalanche sediments. Thus, only the field geomor- phological mapping proved to be reliable for identifying the limits of the paleo-avalanche. The limits identified as granite boulders deposited over volcanic rocks were found to extend 30 m further up the opposite valley slope than previously had been mapped. This larger extent implies a greater volume and/or greater mobility for the prehistoric event. Keywords Slope movements Á Natural hazards Á Schmidt Hammer tests Á Huascaran Á Cordillera Blanca Á Peru 1 Introduction The Cordillera Blanca in Peru is part of the highly tectonically active Andean mountain chain formed by collision of the Cocos, Nazca, Antarctic, and South American lithosphere plates. Intense endogenic processes form suitable conditions for highly active and dan- gerous geomorphic processes.
    [Show full text]
  • How to Cite Complete Issue More Information About This Article
    Sociedade & Natureza ISSN: 0103-1570 ISSN: 1982-4513 Universidade Federal de Uberlândia, Instituto de Geografia, Programa de Pós-Graduação em Geografia Figueiredo, Anderson R. De; Simões, Jefferson C.; Menegat, Rualdo; Strauss, Sarah; Rodrigues, Bruna B. Perceptions of and adaptation to climate change in the Cordillera Blanca, Peru Sociedade & Natureza, vol. 31, e45623, 2019 Universidade Federal de Uberlândia, Instituto de Geografia, Programa de Pós-Graduação em Geografia DOI: https://doi.org/10.14393/SN-v31-2019-45623 Available in: https://www.redalyc.org/articulo.oa?id=321363062020 How to cite Complete issue Scientific Information System Redalyc More information about this article Network of Scientific Journals from Latin America and the Caribbean, Spain and Journal's webpage in redalyc.org Portugal Project academic non-profit, developed under the open access initiative Sociedade & Natureza ISSN: 0103-1570 ISSN: 1982-4513 Universidade Federal de Uberlândia, Instituto de Geografia, Programa de Pós-Graduação em Geografia Perceptions of and adaptation to climate change in the Cordillera Blanca, Peru Figueiredo, Anderson R. De; Simões, Jefferson C.; Menegat, Rualdo; Strauss, Sarah; Rodrigues, Bruna B. Perceptions of and adaptation to climate change in the Cordillera Blanca, Peru Sociedade & Natureza, vol. 31, 2019 Universidade Federal de Uberlândia, Instituto de Geografia, Programa de Pós-Graduação em Geografia Available in: http://www.redalyc.org/articulo.oa?id=321363062020 DOI: 10.14393/SN-v31-2019-45623 PDF generated from XML JATS4R by Redalyc Project academic non-profit, developed under the open access initiative Articles Perceptions of and adaptation to climate change in the Cordillera Blanca, Peru Anderson R. De Figueiredo 1 anderson.fi[email protected] Universidade Federal do Rio Grande do Sul, Brazil Jefferson C.
    [Show full text]