2017 Peru Trip Proposal
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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. -
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 -
Stevie Haston Aleš Česen Malcolm Bass Tom Ballard Steve Skelton F.Lli Franchini Korra Pesce
# 33 Stile Alpino Luoghi & Montagne MONTE BIANCO BHAGIRATHI III CIVETTA KISHTWAR SHIVLING GASHERBRUM IV HIMALAYA MALTA TAULLIRAJU Protagonisti STEVIE HASTON ALEš ČESEN MALCOLM BASS TOM BALLARD STEVE SKELTON F.LLI FRANCHINI KORRA PESCE Speciale PILASTRO ROSSO DEL BROUILLARD In collaborazione con: ALPINE STUDIO EDITORE Trimestrale anno VIII n° 33 settembre 2016 (n. 3/2016) € 4,90 La giacca più leggera e impermeabile del momento LIGHTWEIGHT WITHOUT COMPROMISE MINIMUS 777 JACKET Con un peso di soli 139g, la Minimus 777 è una giacca per Alpinismo e da Trail di una leggerezza estrema, con 3 strati impermeabili, una traspirabilità elevata e una comprimibilità senza precedenti. Pertex® Shield + exclusive technology: 7 denier face, 7 micron membrane, 7 denier tricot backer montane.eu La giacca più leggera e EDITORIAL # 33 impermeabile del momento • Firstly I would like to openly admit that I do not really like to write about or com- ment on other peoples mountaineering endeavors, because it is impossible to comple- tely understand an experience in the mountains unless you have lived it yourself. Ten years after my predecessor I will have the difficult task to replace Fabio Palma in writing the editorials of Stile Alpino. Certainly he is better skilled than me in writing and has been one of the creators of this magazine founded by the Ragni di Lecco group. Nonetheless, I will try to be up to the job helping to select the last ascents around the world and to suggest new places but always taking care to include ascents in the Alps and close to home. The objective of Stile Alpino is to improve and steadily grow in order to publish ar- ticles, that might not have been published before, on ascents in unknown or known areas. -
MONITOREO GLACIOLÓGICO EN EL GLACIAR LLACA Huaraz – Ancash
Ministerio Instituto Nacional de Investigación en Glaciares y del Ambiente Ecosistemas de Montaña “Decenio de las Personas con Discapacidad en el Perú” “Año de la consolidación del Mar de Grau” MONITOREO GLACIOLÓGICO EN EL GLACIAR LLACA Huaraz – Ancash INFORME TÉCNICO N°03 Foto: Oscar Vilca Glaciar Llaca, 2016. Huaraz, Marzo de 2016 1 Ministerio Instituto Nacional de Investigación en Glaciares y del Ambiente Ecosistemas de Montaña “Decenio de las Personas con Discapacidad en el Perú” “Año de la consolidación del Mar de Grau” MINISTERIO DEL AMBIENTE INSTITUTO NACIONAL DE INVESTIGACIÓN EN GLACIARES Y ECOSISTEMAS DE MONTAÑA - INAIGEM INVESTIGACIÓN EN GLACIARES PERSONAL TÉCNICO QUE PARTICIPÓ EN EL INFORME: Ing. Lucas N. Torres Amado. Ing. Luzmila R, Dávila Roller. Ing. Oscar Vilca Gómez. 2 Ministerio Instituto Nacional de Investigación en Glaciares y del Ambiente Ecosistemas de Montaña “Decenio de las Personas con Discapacidad en el Perú” “Año de la consolidación del Mar de Grau” INDICE RESUMEN ........................................................................................................................... 5 I. GENERALIDADES ........................................................................................................ 6 1.1 Introducción .................................................................................................... 6 1.2 Antecedentes .................................................................................................. 6 1.3 Objetivo ......................................................................................................... -
Glaciology in Peru Since 1941
GLACIOLOGY IN PERU SINCE 1941 César Portocarrero [email protected] CLIMATE CHANGES IN THE HUMAN HISTORY THE MEDIEVAL WARMING THE LITLE ICE AGE THE CURRENT GLOBAL WARMING GLACIERS IN PERU GLACIER AREA 71 % IN THE TROPICS 1970 -2,041 km2 2010 ≈ 1,400 km2 Study Area 1.- Cordillera Blanca 2.- Cord. Huallanca 3.- Cord. Huayhuash 4.- Cord. Raura 5.- Cor.Huagoruncho 6.- Cord. La Viuda 7.- Cord. Central 8.- Cord.Huaytapallana 9.- Cord. Chonta 10.- Cord. Ampato 11.- Cord. Urubamba 12.- Cord. Vilcabamba 13.- Cord. Huanzo 14.- Cord. Chila 15.- Cord. La Raya 16.- Cord. Vilcanota 17.- Cord. Carabaya 18.- Cord. Apolobamba - 3,044 glaciers - 2,041.85 Km2 area. 19.- Cord. Volcánica - La Cordillera Blanca con 723 Km2 (35%). CATASTROPHIC EVENTS En 1725 Aluvión que desapareció el pueblo de Ancash En 1725 Avalanchas y aluviones en Huaraz En 1869 Aluvión en Monterrey - Huaraz En 1883 Aluvión en Macashca cerca a Huaraz En 1917 Aluvión del Nevado Huascarán sobre Ranrahirca En 1938 Aluvión en la quebrada Ulta - Carhuaz En 1941 Aluvión en la cuenca del Río Pativilca En 1941 Aluvión en Huaraz - 4 a 5 mil muertos En 1945 Aluvión sobre las ruinas de Chavín de Huantar En 1950 Aluvión en la laguna Jancarurish destruyendo hidroeléctrica En 1951 Primer aluvión en la laguna Artesoncocha – Laguna Parón En 1951 Segundo aluvión en la laguna Artesoncocha - Laguna Parón En 1952 Aluvión en la Laguna Millhuacocha – Quebrada Ishinca En 1953 y 1959 Aluvión en la Laguna Tullparaju – Huaraz En 1962 Aluvión en Ranrahirca del Nevado Huascarán – 4000 muertos En 1965 Aluvión en la Laguna Tumarina – Carhuascancha En 1989 Aluvión en Huancayo procedente de la laguna Chuspicocha En 1970 Aluvión en Yungay y Ranrahirca – 15,000 muertos En 1998 Aluvión de Machupicchu – Destrucción de la Hidroeléctrica HUASCARAN NATIONAL PARK (YELLOW LINE) AND CORDILLERA BLANCA (GLACIERS IN LIGHT BLUE) G. -
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). -
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. -
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. -
A Review of the Current State and Recent Changes of the Andean Cryosphere
feart-08-00099 June 20, 2020 Time: 19:44 # 1 REVIEW published: 23 June 2020 doi: 10.3389/feart.2020.00099 A Review of the Current State and Recent Changes of the Andean Cryosphere M. H. Masiokas1*, A. Rabatel2, A. Rivera3,4, L. Ruiz1, P. Pitte1, J. L. Ceballos5, G. Barcaza6, A. Soruco7, F. Bown8, E. Berthier9, I. Dussaillant9 and S. MacDonell10 1 Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA), CCT CONICET Mendoza, Mendoza, Argentina, 2 Univ. Grenoble Alpes, CNRS, IRD, Grenoble-INP, Institut des Géosciences de l’Environnement, Grenoble, France, 3 Departamento de Geografía, Universidad de Chile, Santiago, Chile, 4 Instituto de Conservación, Biodiversidad y Territorio, Universidad Austral de Chile, Valdivia, Chile, 5 Instituto de Hidrología, Meteorología y Estudios Ambientales (IDEAM), Bogotá, Colombia, 6 Instituto de Geografía, Pontificia Universidad Católica de Chile, Santiago, Chile, 7 Facultad de Ciencias Geológicas, Universidad Mayor de San Andrés, La Paz, Bolivia, 8 Tambo Austral Geoscience Consultants, Valdivia, Chile, 9 LEGOS, Université de Toulouse, CNES, CNRS, IRD, UPS, Toulouse, France, 10 Centro de Estudios Avanzados en Zonas Áridas (CEAZA), La Serena, Chile The Andes Cordillera contains the most diverse cryosphere on Earth, including extensive areas covered by seasonal snow, numerous tropical and extratropical glaciers, and many mountain permafrost landforms. Here, we review some recent advances in the study of the main components of the cryosphere in the Andes, and discuss the Edited by: changes observed in the seasonal snow and permanent ice masses of this region Bryan G. Mark, The Ohio State University, over the past decades. The open access and increasing availability of remote sensing United States products has produced a substantial improvement in our understanding of the current Reviewed by: state and recent changes of the Andean cryosphere, allowing an unprecedented detail Tom Holt, Aberystwyth University, in their identification and monitoring at local and regional scales. -
INVITATION to the ANDES. John C. Oberlin
INVITATION TO THE ANDES INVITATION TO THE ANDES . • BY JOHN C. OBERLIN (Names of mountains printed in italic are unofficial.) ......... Scottish Himalayan Expedition and other similar small parties have stimulated the hopes and aroused the ambitions of young · mountaineers, not only of Great Britain, but also of North America. lt demonstrated that the right sort of amateur party with limited funds could nevertheless explore and· climb in a remote region with eminent satisfaction and success. Many are eager to follow the example. I suggest that the Andes of Peru may offer what they seek. Peru ~s a magnificent country, bounded by the Pacific Ocean to the west but largely draining into the Atlantic. This apparent anomaly is due to the extensive series of mountain ranges relatively near the coast which rise above 2o,ooo ft. and separate the strip of dry coastal plain from the luxuriant forests of the Amazon basin. .Most of the higher peaks are sheathed in snow and ice and many remain unclimbed despite the ready accessibility of their bases, for the simple reason that they are both difficult and dangerous. Other very large peaks, such as the volcano Coropuna (6,613 m.), offer no real problem other than their size. If the proper time of year is s~lected the weather is both com fortable and reliable, despite proximity to the equator, due to the effect of the cold Humboldt Current along· the coast and to the altitude of the valleys from which the peaks are reached. The Peruvians are friendly and most hospitable, and living and travel expenses are low.