Peruvian Andes Expedition 2018 Imperial College London Exploration Board Report
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1 Curry Slaymaker
Curry Slaymaker - Father of Huascarán National Park By Lew Scholl Originally dated 7/2/2009 Updated 3/29/2011 [email protected] This year (2011) is the 50th anniversary of the Peace Corps. Its accomplishments are being recognized in many places around the world that have hosted Peace Corps volunteers. As one who has traveled and climbed in Peru, I have a particular interest in one Peace Corps volunteer who accomplished something that those of us who love the mountains consider truly noteworthy; the creation of a major national park in one of the world’s most spectacular mountain ranges, Peru’s Cordillera Blanca – (the White Range”). Curry Slaymaker, who grew up in Rainier Oregon, laid the groundwork for Huascarán National Park while in the Peace Corps. In 1972, six years after leaving the Peace Corps, driven by his deep love of this magnificent place, he came back again to complete this work as a direct employee of the Peruvian government. In 1973, while traveling in Peru, I had the opportunity to meet him. In 1976 he died in a mountaineering accident only a year after the park had become a reality, largely under his guidance and inspiration. This history and Curry’s accomplishments are little known outside of Peru. In 2007 I joined in a Mazama outing and trek around Peru’s Huayhuash Range – a trip that took us to Huaraz, the mountaineering “Mecca” of the Cordillera Blanca and Peru. This trip inspired me to investigate Curry’s life and the circumstances of his death. What follows is the result of that research. -
Nobody Knows Anything Two New Routes in the Cordillera Blanca of Peru
AAC Publications Nobody Knows Anything Two New Routes in the Cordillera Blanca of Peru THE IDEA of going to Peru wasn’t sparked by some coveted unclimbed line. It was simply out of convenience and practicality. As the winter season in the Canadian Rockies wound down, I was getting antsy to go on a trip. Peru seemed ideal: big mountains in a country I had never visited, a chance to see how my body did at altitude, with simple logistics and low costs to boot. My schedule would allow me a month to “train” (i.e., go climbing), and I could go right in the middle of Peru’s dry season. Finding a willing partner with the same open schedule proved more challenging, but eventually I convinced my friend Quentin Lindfield Roberts to take three weeks off. I booked a ticket for six weeks, with no clear plan for the second half of my trip. Upon arriving in Huaraz, Quentin and I quickly found our favorite breakfast hang at Café Andino. Over an endless stream of espresso, we bounced ideas off each other for what to do with his brief time in the country. Eventually we agreed to acclimatize in the Santa Cruz Valley and then consider trying something new. We departed a day later with packs light on climbing gear and heavy with good food, wondering why we’d decided not to cough up the $20 to get our loads hauled in on burros. After a rest day in Alpamayo base camp and a riveting game of bocce ball among the boulders at the moraine camp, at 5,000 meters, we slogged up to the Alpamayo-Quitaraju col, where we decided we still had enough daylight and energy to head up Alpamayo that afternoon. -
Water, Silt and Dams: Prehispanic Geological Storage in the Cordillera
Water, Silt and Dams: Prehispanic Geological Storage in the Cordillera Negra, North-Central Andes, Peru Agua, Limo y Represas: Almacenaje Geológico Prehispánico en la Cordillera Negra, Andes Norcentrales, Perú Kevin Lane1 ([email protected]) 1CONICET - Instituto de Arqueología, Facultad de Filosofía y Letras, Universidad de Buenos Aires, Argentina https://doi.org/10.36580/rgem.i2.41-50 …Y después mandó los señores reyes ingas guardar la costumbre y ley de que no meneasen todas las dichas acequias, agua de regar las dichas sementeras, hasta los pastos de ganado regaban en los altos y quebradas… (Guaman Poma de Ayala, 1993 [1615],780) Abstract a las dificultades en mantener un flujo regular de agua, especialmente durante la estación seca, esto constituye una Over the past few decades there has been an increasing respuesta lógica a una necesidad urgente. Sin embargo, la interest in building micro-dams across the whole of the falta de agua no es un fenómeno moderno, es un problema Cordillera Negra, North-Central Andes, Peru. Given the de larga data que se abordó de forma similar en el pasado. difficulties in maintaining a regular flow of water, especially Por lo tanto, el conocimiento del paisaje y las habilidades during the dry season, it is a logical response to a pressing indígenas llevaron a la selección de sitios para hacer need. Yet, lack of water is not a modern phenomenon, it is a represas. long-standing problem that was tackled in a similar fashion in the past. Then, indigenous skill and landscape knowhow Los ingenieros modernos han seguido su ejemplo, informed the selection of sites for damming. -
Time and Mode of Exhumation of the Cordillera Blanca Batholith
Time and mode of exhumation of the Cordillera Blanca batholith (Peruvian Andes) Audrey Margirier, Laurence Audin, Xavier Robert, Frédéric Herman, Jérôme Ganne, Stephane Schwartz To cite this version: Audrey Margirier, Laurence Audin, Xavier Robert, Frédéric Herman, Jérôme Ganne, et al.. Time and mode of exhumation of the Cordillera Blanca batholith (Peruvian Andes). Journal of Geophysical Research : Solid Earth, American Geophysical Union, 2016, 121 (8), pp.6235-6249. 10.1002/2016JB013055. insu-01677067 HAL Id: insu-01677067 https://hal-insu.archives-ouvertes.fr/insu-01677067 Submitted on 7 Jan 2018 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. PUBLICATIONS Journal of Geophysical Research: Solid Earth RESEARCH ARTICLE Time and mode of exhumation of the Cordillera 10.1002/2016JB013055 Blanca batholith (Peruvian Andes) Key Points: Audrey Margirier1, Laurence Audin1, Xavier Robert1, Frédéric Herman2, Jérôme Ganne3, • First thermobarometry data in the 1 Cordillera Blanca batholith indicates and Stéphane Schwartz its emplacement in the upper crust 1 -
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 -
An Introduction to the Bofedales of the Peruvian High Andes
An introduction to the bofedales of the Peruvian High Andes M.S. Maldonado Fonkén International Mire Conservation Group, Lima, Peru _______________________________________________________________________________________ SUMMARY In Peru, the term “bofedales” is used to describe areas of wetland vegetation that may have underlying peat layers. These areas are a key resource for traditional land management at high altitude. Because they retain water in the upper basins of the cordillera, they are important sources of water and forage for domesticated livestock as well as biodiversity hotspots. This article is based on more than six years’ work on bofedales in several regions of Peru. The concept of bofedal is introduced, the typical plant communities are identified and the associated wild mammals, birds and amphibians are described. Also, the most recent studies of peat and carbon storage in bofedales are reviewed. Traditional land use since prehispanic times has involved the management of water and livestock, both of which are essential for maintenance of these ecosystems. The status of bofedales in Peruvian legislation and their representation in natural protected areas and Ramsar sites is outlined. Finally, the main threats to their conservation (overgrazing, peat extraction, mining and development of infrastructure) are identified. KEY WORDS: cushion bog, high-altitude peat; land management; Peru; tropical peatland; wetland _______________________________________________________________________________________ INTRODUCTION organic soil or peat and a year-round green appearance which contrasts with the yellow of the The Tropical Andes Cordillera has a complex drier land that surrounds them. This contrast is geography and varied climatic conditions, which especially striking in the xerophytic puna. Bofedales support an enormous heterogeneity of ecosystems are also called “oconales” in several parts of the and high biodiversity (Sagástegui et al. -
CARMEN SALCEDO Anta Viscahuayjo Viscahuaycco Emboquillado, Una Via Choccetucro CHIPAO Trocha, Autopista LUCANAS 30 Tocsa Trocha, Una Via PUQUIO
S 74° W S ° ° 2 CONCEPCION 2 1 590000 595000 600000 605000 610000 615000 620000 625000 1 CHUPACA JUNIN Comunidad Campesina Trapiche Jarhuaymarca JUNIN SATIPO Mayo o Luren Chullumpi Peccollay Lliulliscca Pucche Villavista TAYACAJA HUANCAYO Telarhuasi Yanasora Comunidad Campesina Putacca Aucara Irahua HUANTA Saccrahua AY Ccaccatuna ¬1083 CHURCAMPA « CUSCO HUANCAVELICA Cachi LA CONVENCION ACOBAMBA Huantaymisa HUANCAVELICA LA MAR Pisccapuquio ANGARAES Corita Huancaccocha Kichka CASTROVIRREYNA Taxapacocha 75 Curita / Corita URUBAMBA Pacocha HUAMANGA Emp. PE-32 A (Cabana) Huantaymisa. CANGALLO Huantaymisa Millpocc CHINCHEROS ANTA 90 Laguna Tayapampa HUAYTARA VILCAS Lliullisja HUAMAN Tayapampa AY VICTOR FAJARDO Siniega Cucho Tantar Pucro 1078 ANDAHUAYLAS µLaguna «¬ 0 0 ABANCAY Huancaccocha Paca 0 0 APURIMAC AY HUANCA 0 0 S S SANCOS ° 5 1133 5 ° 4 4 1 «¬ 1 1 1 4 4 ICA GRAU 8 8 SUCRE Pacha Pucuna Acco Pite o Huancapampa. ay M CARMEN o Choqueccocha gr Huancapampa / Huancapay ICA Ne SALCEDO o Jatun Puquio Rí Accenta AYMARAES ANTABAMBA Roque PALPA 4182 Ñahuinpuquio Chuño Ccara LUCANAS AYACUCHO Cullo Pampa Chupahuaijo Laguna Chaquejocha 70 Pasjopuquio Conty Huaycco Huanahuire NASCA PARINACOCHAS Capillayocc PAUCAR DEL LA UNION Capillayocc Ccaray Huillacconcco SARA SARA Ajopita Jechjaypampa Allhiscca Laguna AY AREQUIPA Agornichayoc 1087 CARAVELI Laguna CARMEN Yanaccocha «¬ OCÉANO Laguna Rayosjocha AY Parccacocha Huana SALCEDO Parccacha PACÍFICO Huire 1078 Colpachayoc / Ccolpachacon Huilaccota «¬ CASTILLA CONDESUYOS Ccollpapampa Chiro Chiro 74° W Quipampampa Ccana Chacca Emp. AY-1084 Ccolcca Sorapampa Ccelluaccasa Huasa Lucre AY CHIPAO Chipao «¬1084 Emp. AY-1066 Piruro Huaycco Huasapampa R í o Chillmay Mio Ccollpa Chipao Usccamarca M a LUCANAS y o 95 b a m R Yarpo b Culluauayjo a ío L Chuquio Huanca Pampa liu CABANA l Huillque Ñuñorjoparja lis ja Emp. -
Landsat TM and ETM+ Derived Snowline Altitudes in the Cordillera Huayhuash and Cordillera Raura, Peru, 1986–2005
The Cryosphere, 5, 419–430, 2011 www.the-cryosphere.net/5/419/2011/ The Cryosphere doi:10.5194/tc-5-419-2011 © Author(s) 2011. CC Attribution 3.0 License. Landsat TM and ETM+ derived snowline altitudes in the Cordillera Huayhuash and Cordillera Raura, Peru, 1986–2005 E. M. McFadden1,*,**, J. Ramage1, and D. T. Rodbell2 1Earth and Environmental Sciences, Lehigh University, 1 West Packer Ave., Bethlehem, PA 18015, USA 2Geology Department, Union College, Schenectady, NY 12308, USA *now at: Byrd Polar Research Center, The Ohio State University, 1090 Carmack Road, Columbus, OH 43210, USA **now at: School of Earth Sciences, The Ohio State University, 275 Mendenhall Laboratory, 125 S. Oval Mall, Columbus, OH 43210, USA Received: 13 August 2010 – Published in The Cryosphere Discuss.: 6 October 2010 Revised: 10 March 2011 – Accepted: 4 May 2011 – Published: 23 May 2011 Abstract. The Cordilleras Huayhuash and Raura are remote and better-known Cordillera Blanca, and has 117 glaciers glacierized ranges in the Andes Mountains of Peru. A robust covering ∼85 km2 (Morales Arnao, 2001). Peaks are typ- assessment of modern glacier change is important for under- ically over 6000 m a.s.l., with the highest peak recorded at standing how regional change affects Andean communities, 6617 m a.s.l. (Nevado Yerupaja).´ The Cordillera Raura, lo- and for placing paleo-glaciers in a context relative to mod- cated to the southeast of the Cordillera Huayhuash, has ern glaciation and climate. Snowline altitudes (SLAs) de- a slightly smaller (55 km2) glacier area (Morales Arnao, rived from satellite imagery are used as a proxy for modern 2001). -
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). -
Pdf/77-Wrvw-272.Pdf
H-ART. Revista de historia, teoría y crítica de arte ISSN: 2539-2263 ISSN: 2590-9126 [email protected] Universidad de Los Andes Colombia Ambrosino, Gordon Inscription, Place, and Memory: Palimpsest Rock Art and the Evolution of Highland, Andean Social Landscapes in the Formative Period (1500 – 200 BC) H-ART. Revista de historia, teoría y crítica de arte, no. 5, 2019, July-, pp. 127-156 Universidad de Los Andes Colombia DOI: https://doi.org/10.25025/hart05.2019.07 Available in: https://www.redalyc.org/articulo.oa?id=607764857003 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 Inscription, Place, and Memory: Palimpsest Rock Art and the Evolution of Highland, Andean Social Landscapes in the Formative Period (1500 – 200 BC) Inscripción, lugar y memoria: arte rupestre palimpsesto y la evolución de los paisajes sociales andinos en las tierras altas durante el Período Formativo (1500 - 200 a. C.) Inscrição, local e memória: arte de uma roca palimpsesto e a evolução das paisagens sociais andinas durante o Período Formativo (1500 - 200 a. e. c.) Received: January 27, 2019. Accepted: April 12, 2019. Modifications: April 24, 2019 DOI: https://doi.org/10.25025/hart05.2019.07 Gordon Ambrosino Abstract Mellon Postdoctoral Curatorial Fellow, Los Angeles As more than a means of recalling, memory is an active County Museum of Art, Los Angeles, Art of the Ancient cultural creation and landscape inscriptions construct Americas Department. -
Holocene Glacier Fluctuations
Quaternary Science Reviews 111 (2015) 9e34 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Invited review Holocene glacier fluctuations * Olga N. Solomina a, b, , Raymond S. Bradley c, Dominic A. Hodgson d, Susan Ivy-Ochs e, f, Vincent Jomelli g, Andrew N. Mackintosh h, Atle Nesje i, j, Lewis A. Owen k, Heinz Wanner l, Gregory C. Wiles m, Nicolas E. Young n a Institute of Geography RAS, Staromonetny-29, 119017, Staromonetny, Moscow, Russia b Tomsk State University, Tomsk, Russia c Department of Geosciences, University of Massachusetts, Amherst, MA 012003, USA d British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK e Institute of Particle Physics, ETH Zurich, 8093 Zurich, Switzerland f Institute of Geography, University of Zurich, 8057 Zurich, Switzerland g Universite Paris 1 Pantheon-Sorbonne, CNRS Laboratoire de Geographie Physique, 92195 Meudon, France h Antarctic Research Centre, Victoria University Wellington, New Zealand i Department of Earth Science, University of Bergen, N-5020 Bergen, Norway j Uni Research Klima, Bjerknes Centre for Climate Research, N-5020 Bergen Norway k Department of Geology, University of Cincinnati, Cincinnati, OH 45225, USA l Institute of Geography and Oeschger Centre for Climate Change Research, University of Bern, Switzerland m Department of Geology, The College of Wooster, Wooster, OH 44691, USA n Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY, USA article info abstract Article history: A global overview of glacier advances and retreats (grouped by regions and by millennia) for the Received 15 July 2014 Holocene is compiled from previous studies. The reconstructions of glacier fluctuations are based on Received in revised form 1) mapping and dating moraines defined by 14C, TCN, OSL, lichenometry and tree rings (discontinuous 22 November 2014 records/time series), and 2) sediments from proglacial lakes and speleothems (continuous records/ Accepted 27 November 2014 time series). -
A Journey Through the Cordillera Blanca of Peru
88 A JOURNEY THROUGH THE CORDILLERA BLANCA OF PERU A JOURNEY THROUGH THE CORDILLERA BLANCA OF PERU BY H. L. STEMBRIDGE (Six illustrations: nos. 30- 35) • F the nine weeks that Alf Gregory and I were together in Peru in the middle of 1963 five were spent among the mountains of the Cordillera Blanca, two in the 'hotlands ', the lush, humid forests bordering the Alto Madre de Dios river, the remainder in the central uplands where the great ruined cities of the Incas ar.e to be found. Each phase had its attractions. If the ruins enthralled us, the jungle~ was far and away the most amusing, though a trifle uncomfortable, but for unalloyed pleasure a three weeks' journey through the Cordillera Blanca takes pride of place. I suppose that most of us, at some period in our lives, find that the urge to lay siege to a peak diminishes that our happiness among mountains spreads itself to embrace everything that surrounds them, that to travel along the valleys and ridges and over the passes camping, photographing, meeting a people whose history and customs intrigue us, gives to us as much pleasure as do the mountains we manage to scale. For people who enjoy this sort of thing, there can be nothing better than the Cordillera Blanca. Greg says the peaks there are as fine as any in the world, and he should know. Equally impressive were the accessories the flowers in late spring, more colourful than the Alps, birds amazing in variety, a climate set fair from May to August, unexploited antiquities and, of course, the Indians, primitive, splendid, colourful, dirty, completely uninhibited ,.---most of all the Indians.