Peruvian Andes Adventures Guide & Driver
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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. -
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. -
Relación De Agencias Que Atenderán De Lunes a Viernes De 8:30 A. M. a 5:30 P
Relación de Agencias que atenderán de lunes a viernes de 8:30 a. m. a 5:30 p. m. y sábados de 9 a. m. a 1 p. m. (con excepción de la Ag. Desaguadero, que no atiende sábados) DPTO. PROVINCIA DISTRITO NOMBRE DIRECCIÓN Avenida Luzuriaga N° 669 - 673 Mz. A Conjunto Comercial Ancash Huaraz Huaraz Huaraz Lote 09 Ancash Santa Chimbote Chimbote Avenida José Gálvez N° 245-250 Arequipa Arequipa Arequipa Arequipa Calle Nicolás de Piérola N°110 -112 Arequipa Arequipa Arequipa Rivero Calle Rivero N° 107 Arequipa Arequipa Cayma Periférica Arequipa Avenida Cayma N° 618 Arequipa Arequipa José Luis Bustamante y Rivero Bustamante y Rivero Avenida Daniel Alcides Carrión N° 217A-217B Arequipa Arequipa Miraflores Miraflores Avenida Mariscal Castilla N° 618 Arequipa Camaná Camaná Camaná Jirón 28 de Julio N° 167 (Boulevard) Ayacucho Huamanga Ayacucho Ayacucho Jirón 28 de Julio N° 167 Cajamarca Cajamarca Cajamarca Cajamarca Jirón Pisagua N° 552 Cusco Cusco Cusco Cusco Esquina Avenida El Sol con Almagro s/n Cusco Cusco Wanchaq Wanchaq Avenida Tomasa Ttito Condemaita 1207 Huancavelica Huancavelica Huancavelica Huancavelica Jirón Francisco de Angulo 286 Huánuco Huánuco Huánuco Huánuco Jirón 28 de Julio N° 1061 Huánuco Leoncio Prado Rupa Rupa Tingo María Avenida Antonio Raymondi N° 179 Ica Chincha Chincha Alta Chincha Jirón Mariscal Sucre N° 141 Ica Ica Ica Ica Avenida Graú N° 161 Ica Pisco Pisco Pisco Calle San Francisco N° 155-161-167 Junín Huancayo Chilca Chilca Avenida 9 De Diciembre N° 590 Junín Huancayo El Tambo Huancayo Jirón Santiago Norero N° 462 Junín Huancayo Huancayo Periférica Huancayo Calle Real N° 517 La Libertad Trujillo Trujillo Trujillo Avenida Diego de Almagro N° 297 La Libertad Trujillo Trujillo Periférica Trujillo Avenida Manuel Vera Enríquez N° 476-480 Avenida Victor Larco Herrera N° 1243 Urbanización La La Libertad Trujillo Victor Larco Herrera Victor Larco Merced Lambayeque Chiclayo Chiclayo Chiclayo Esquina Elías Aguirre con L. -
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 -
Redalyc.Railroads in Peru: How Important Were They?
Desarrollo y Sociedad ISSN: 0120-3584 [email protected] Universidad de Los Andes Colombia Zegarra, Luis Felipe Railroads in Peru: How Important Were They? Desarrollo y Sociedad, núm. 68, diciembre, 2011, pp. 213-259 Universidad de Los Andes Bogotá, Colombia Available in: http://www.redalyc.org/articulo.oa?id=169122461007 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Revista 68 213 Desarrollo y Sociedad II semestre 2011 Railroads in Peru: How Important Were They? Ferrocarriles en el Perú: ¿Qué tan importantes fueron? Luis Felipe Zegarra* Abstract This paper analyzes the evolution and main features of the railway system of Peru in the 19th and early 20th centuries. From mid-19th century railroads were considered a promise for achieving progress. Several railroads were then built in Peru, especially in 1850-75 and in 1910-30. With the construction of railroads, Peruvians saved time in travelling and carrying freight. The faster service of railroads did not necessarily come at the cost of higher passenger fares and freight rates. Fares and rates were lower for railroads than for mules, especially for long distances. However, for some routes (especially for short distances with many curves), the traditional system of llamas remained as the lowest pecuniary cost (but also slowest) mode of transportation. Key words: Transportation, railroads, Peru, Latin America. JEL classification: N70, N76, R40. * Luis Felipe Zegarra is PhD in Economics of University of California at Los Angeles (UCLA). -
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. -
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). -
Locales De Votación Al 17-01-2020
LOCALES DE VOTACIÓN AL VIERNES 17 DE ENERO DE 2020 Llámanos gratis al 0800-79-100 Todos los días de 06:00 hasta 22:00 horas Presiona CONTROL + F para buscar tu local. N° ODPE NOMBRE ODPE SEDE DE ODPE UBIGEO DEPARTAMENTO PROVINCIA DISTRITO ID LOCAL NOMBRE DEL LOCAL DIRECCIÓN DEL LOCAL MESAS ELECTORES CCPP TIPO TECNOLOGÍA VRAEM 1 1 BAGUA BAGUA 010201 AMAZONAS BAGUA LA PECA 0025 IE 16281 AV. BAGUA SN 1 104 ESPITAL CON 2 1 BAGUA BAGUA 010201 AMAZONAS BAGUA LA PECA 0026 IE 16277 JR. PROGRESO SN 1 147SAN ISIDRO CON 3 1 BAGUA BAGUA 010201 AMAZONAS BAGUA LA PECA 0027 IE 31 NUESTRA SEÑORA DE GUADALUPE - FE Y ALEGRIA JR. MARAÑÓN SN 15 4243 CON 4 1 BAGUA BAGUA 010201 AMAZONAS BAGUA LA PECA 0028 IE 16275 AV. SAN FELIPE N° 486 8 2237 CON 5 1 BAGUA BAGUA 010201 AMAZONAS BAGUA LA PECA 0029 IE 16279 AV. LA FLORIDA SN 2 312ARRAYAN CON 6 1 BAGUA BAGUA 010201 AMAZONAS BAGUA LA PECA 0030 IE 16283 AV. CORONEL BENITES SN 1 184 CHONZA ALTA CON 7 1 BAGUA BAGUA 010201 AMAZONAS BAGUA LA PECA 5961 IE 16288 AV. ATAHUALPA SN 2 292SAN FRANCISCO CON 8 1 BAGUA BAGUA 010202 AMAZONAS BAGUA ARAMANGO 0032 IE MIGUEL MONTEZA TAFUR AV. 28 DE JULIO SN 8 2402 SEA 9 1 BAGUA BAGUA 010202 AMAZONAS BAGUA ARAMANGO 0033 IE 16201 AV. 28 DE JULIO SN 18 5990 SEA 10 1 BAGUA BAGUA 010203 AMAZONAS BAGUA COPALLIN 0034 IE 16239 JR. RODRIGUEZ DE MENDOZA N° 651 15 4142 CON 11 1 BAGUA BAGUA 010204 AMAZONAS BAGUA EL PARCO 0035 IE 16273 JR. -
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).