Inca Mountaintop Shrines and Glaciers in the High Andes
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Andinismo: Desafío Para La Prensa Nacional Memoria Para Optar Al Título De Periodista
UNIVERSIDAD NACIONAL 11111111111111�ñi�íll1i1i1l1lm1111111111111 35612000064981. UNIVERSIDADa ANDRES BELLO UNIVERSIDAD ANDRÉS BELLO FACULTAD DE HUMANIDADES Y EDUCACIÓN ESCUELA DE PERIODISMO ANDINISMO: DESAFÍO PARA LA PRENSA NACIONAL MEMORIA PARA OPTAR AL TÍTULO DE PERIODISTA ALUMNO: CARLA BERTOSSI ARRIBADA PROFESOR GUÍA: SEBASTIANO BERTOLONE GALLETINI SANTIAGO - CHILE Noviembre, 2004 ÍNDICE Justificacióndel Tema ............................................................................................ 2 ANDINISMO: DESAFÍO PARA LA PRENSA NACIONAL ............................................ 4 Introducción............... ......................................................................................... 5 Capítulo I CARACTERÍSTICAS FÍSICAS DE LOS ANDES ......................................................... 8 1. Geografia de Los Andes 2. El ambientede montaña 3. Cumbres emblemáticas Capítulo II MONTAÑAS, TEMPLO DEL DEPORTE.................................................................. 29 l. Breve historia del andinismo 2. El deporte de montaña 3. Andinismo 4. Organización del andinismo en Chile Capítulo m TÉCNICA Y SEGURIDAD EN MONTAÑA.............................................................. 50 l. Peligros en montaña 2. Vestuarioy equipo de montaña 3. Alimentación 4. Orientación Capítulo IV FISIOLOGÍA DE MONTAÑA ................................................................................ 69 1. Patología de la altitud 2. Aclimatización 3. Otraspatologías 4. Primeros auxilios 5. Aspectos psicológicos Capítulo V ACCIDENTES -
Mitigation of Environmental Extremes As a Possible Indicator of Extended Habitat Sustainability for Lakes on Early Mars
Invited Paper Mitigation of Environmental Extremes as a Possible Indicator of Extended Habitat Sustainability for Lakes on Early Mars Nathalie A. Cabrol*a, Edmond A. Grina, Andrew N. Hockb aNASA Ames Research Center/SETI Carl Sagan Center, Space Science Division, MS 245-3. Moffett Field, CA 94035- 1000, USA; bUCLA. Dpt. of Earth & Space Sciences. 595 Charles Young Drive East, Los Angeles, CA 90095-1567. ABSTRACT The impact of individual extremes on life, such as UV radiation (UVR), temperatures, and salinity is well documented. However, their combined effect in nature is not well-understood while it is a fundamental issue controlling the evolution of habitat sustainability within individual bodies of water. Environmental variables combine in the Bolivian Altiplano to produce some of the highest, least explored and most poorly understood lakes on Earth. Their physical environment of thin atmosphere, high ultraviolet radiation, high daily temperature amplitude, ice, sulfur-rich volcanism, and hydrothermal springs, combined with the changing climate in the Andes and the rapid loss of aqueous habitat provide parallels to ancient Martian lakes at the Noachian/Hesperian transition 3.7-3.5 Ga ago. Documenting this analogy is one of the focuses of the High-Lakes Project (HLP). The geophysical data we collected on three of them located up to 5,916 m elevation suggests that a combination of extreme factors does not necessarily translate into a harsher environment for life. Large and diverse ecosystems adapt to UVR reaching 200%-216% that of sea level in bodies of water sometimes no deeper than 50 cm, massive seasonal freeze-over, and unpredictable daily evolution of UVR and temperature. -
Andean Textile Traditions: Material Knowledge and Culture, Part 1 Elena Phipps University of California, Los Angeles, [email protected]
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln PreColumbian Textile Conference VII / Jornadas de Centre for Textile Research Textiles PreColombinos VII 11-13-2017 Andean Textile Traditions: Material Knowledge and Culture, Part 1 Elena Phipps University of California, Los Angeles, [email protected] Follow this and additional works at: http://digitalcommons.unl.edu/pct7 Part of the Art and Materials Conservation Commons, Chicana/o Studies Commons, Fiber, Textile, and Weaving Arts Commons, Indigenous Studies Commons, Latina/o Studies Commons, Museum Studies Commons, Other History of Art, Architecture, and Archaeology Commons, and the Other Languages, Societies, and Cultures Commons Phipps, Elena, "Andean Textile Traditions: Material Knowledge and Culture, Part 1" (2017). PreColumbian Textile Conference VII / Jornadas de Textiles PreColombinos VII. 10. http://digitalcommons.unl.edu/pct7/10 This Article is brought to you for free and open access by the Centre for Textile Research at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in PreColumbian Textile Conference VII / Jornadas de Textiles PreColombinos VII by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Andean Textile Traditions: Material Knowledge and Culture, Part 1 Elena Phipps In PreColumbian Textile Conference VII / Jornadas de Textiles PreColombinos VII, ed. Lena Bjerregaard and Ann Peters (Lincoln, NE: Zea Books, 2017), pp. 162–175 doi:10.13014/K2V40SCN Copyright © 2017 by the author. Compilation copyright © 2017 Centre for Textile Research, University of Copenhagen. 8 Andean Textile Traditions: Material Knowledge and Culture, Part 1 Elena Phipps Abstract The development of rich and complex Andean textile traditions spanned millennia, in concert with the development of cul- tures that utilized textiles as a primary form of expression and communication. -
Pre-Departure Information
Pre-Departure Information DISCOVERING PERU AND BOLIVIA Table of Contents TRAVEL INFORMATION Passport Visas Money Tipping Special Diets Communications Electricity MEDICAL INFORMATION Inoculations International Health Card Malaria Prevention (For Rainforest Extension Only) Staying Healthy HELPFUL INFORMATION Photography Being a Considerate Traveler Words and Phrases PACKING LIST The Essentials WT Gear Store Luggage Weight Limits Notes on Clothing Equipment Personal First Aid Supplies Optional Items READING LIST Essential Reading Also Recommended Reminders Before You Go WELCOME! We’re delighted to welcome you on this adventure! This booklet is designed to guide you in the practical details for preparing for your trip. As you read, if any questions come to mind, feel free to give us a call or send us an email—we’re here to help. PLEASE SEND US Trip Application: Complete, sign, and return your Trip Application form as soon as possible if you have not already done so. Medical Form: Complete, sign, and return your Medical Form as soon as possible if you have not already done so. Air Schedule: Please forward a copy of your email confirmation, which shows your exact flight arrival and departure times. Refer to the Arrival & Departure section of the Detailed Itinerary for instructions. Please feel free to review your proposed schedule with Wilderness Travel before purchasing your tickets if you have any questions about the timing of your arrival and departure flights or would like to confirm we have the required minimum number of participants to operate the trip. Passport Photocopy: Scan* a COLOR copy of your passport photo page and email it to us as a JPG or PDF attachment, or send us a high quality photocopy by mail (immediately upon reserving your trip). -
Rapid Magma Ascent and Generation of Th Excesses in the Lower Crust At
Earth and Planetary Science Letters 255 (2007) 229–242 www.elsevier.com/locate/epsl Rapid magma ascent and generation of 230Th excesses in the lower crust at Puyehue–Cordón Caulle, Southern Volcanic Zone, Chile ⁎ Brian R. Jicha a, , Brad S. Singer a, Brian L. Beard a, Clark M. Johnson a, Hugo Moreno-Roa b,c, José Antonio Naranjo b a Department of Geology and Geophysics, University of Wisconsin—Madison, 1215 West Dayton Street, Madison WI 53706, USA b Servicio Nacional de Geología y Minería (SERNAGEOMIN), Avenida Santa María, 0104 Santiago, Chile c Observatorio Volcanologico de los Andes del Sur (OVDAS), Cerro Ñielol-Sector Antenas, Temuco, Chile Received 28 July 2006; received in revised form 7 December 2006; accepted 8 December 2006 Available online 30 January 2007 Editor: R.W. Carlson Abstract Basaltic to rhyolitic lavas and tephras erupted over the last 70 kyr at the Puyehue–Cordón Caulle volcanic complex in the Andean Southern Volcanic Zone (SVZ) were analyzed for major and trace element, Sr isotope, and U–Th isotope compositions to constrain the timescales of magmatic processes and identify the subducted and crustal components involved in magma genesis. Internal U–Th mineral isochrons from five lavas and three tephra fall deposits are indistinguishable from their eruption ages, indicating a short period (b1000 yr) of crystal residence in the magma prior to eruption. The (230Th/232Th) ratios define a narrow range (0.80–0.83) compared to that of all SVZ lavas (0.72–0.97), suggesting that Puyehue basalt was derived from a relatively uniform mantle source. Dacites and rhyolites have the largest U excesses and likely evolved via fractional crystallization of a plagioclase-dominated mineral assemblage. -
Multiple Sources for Tephra from AD 1259 Volcanic Signal in Antarctic Ice
Multiple sources for tephra from AD 1259 volcanic signal in Antarctic ice cores Biancamaria Narcisi, Jean Robert Petit, Barbara Delmonte, Valentina Batanova, Joel Savarino To cite this version: Biancamaria Narcisi, Jean Robert Petit, Barbara Delmonte, Valentina Batanova, Joel Savarino. Mul- tiple sources for tephra from AD 1259 volcanic signal in Antarctic ice cores. Quaternary Science Reviews, Elsevier, 2019, 210, pp.164-174. 10.1016/j.quascirev.2019.03.005. hal-02350371 HAL Id: hal-02350371 https://hal.archives-ouvertes.fr/hal-02350371 Submitted on 25 Nov 2020 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. Manuscript Details Manuscript number JQSR_2019_21 Title MULTIPLE SOURCES FOR TEPHRA FROM AD 1259 VOLCANIC SIGNAL IN ANTARCTIC ICE CORES Abstract Strong volcanic signals simultaneously recorded in polar ice sheets are commonly assigned to major low-latitude eruptions that dispersed large quantities of aerosols in the global atmosphere with the potential of inducing climate perturbations. Parent eruptions responsible for specific events are typically deduced from matching to a known volcanic eruption having coincidental date. However, more robust source linkage can be achieved only through geochemical characterisation of the airborne volcanic glass products (tephra) sometimes preserved in the polar strata. -
Redalyc.Geochemistry, U-Pb SHRIMP Zircon Dating and Hf Isotopes of The
Andean Geology ISSN: 0718-7092 [email protected] Servicio Nacional de Geología y Minería Chile Poma, Stella; Zappettini, Eduardo O.; Quenardelle, Sonia; Santos, João O.; Koukharsky, Magdalena; Belousova, Elena; McNaughton, Neil Geochemistry, U-Pb SHRIMP zircon dating and Hf isotopes of the Gondwanan magmatism in NW Argentina: petrogenesis and geodynamic implications Andean Geology, vol. 41, núm. 2, mayo, 2014, pp. 267-292 Servicio Nacional de Geología y Minería Santiago, Chile Available in: http://www.redalyc.org/articulo.oa?id=173931252001 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 Andean Geology 41 (2): 267-292. May, 2014 Andean Geology doi: 10.5027/andgeoV41n2-a01 formerly Revista Geológica de Chile www.andeangeology.cl Geochemistry, U-Pb SHRIMP zircon dating and Hf isotopes of the Gondwanan magmatism in NW Argentina: petrogenesis and geodynamic implications Stella Poma1, Eduardo O. Zappettini 2, Sonia Quenardelle 1, João O. Santos 3, † Magdalena Koukharsky 1, Elena Belousova 4, Neil McNaughton 3 1 Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires (IGEBA-CONICET), Universidad de Buenos Aires, Facultad de Ciencias Exactas y Naturales, Departamento de Ciencias Geológicas, Pabellón II-Ciudad Universitaria, Intendente Güiraldes 2160, C1428 EGA, Argentina. [email protected]; [email protected] 2 Servicio Geológico Minero Argentino (SEGEMAR), Avda. General Paz 5445, edificio 25, San Martín B1650WAB, Argentina. [email protected] 3 University of Western Australia, 35 Stirling Highway, Crawley WA 6009, Australia. -
Evaluación Del Riesgo Volcánico En El Sur Del Perú
EVALUACIÓN DEL RIESGO VOLCÁNICO EN EL SUR DEL PERÚ, SITUACIÓN DE LA VIGILANCIA ACTUAL Y REQUERIMIENTOS DE MONITOREO EN EL FUTURO. Informe Técnico: Observatorio Vulcanológico del Sur (OVS)- INSTITUTO GEOFÍSICO DEL PERÚ Observatorio Vulcanológico del Ingemmet (OVI) – INGEMMET Observatorio Geofísico de la Univ. Nacional San Agustín (IG-UNSA) AUTORES: Orlando Macedo, Edu Taipe, José Del Carpio, Javier Ticona, Domingo Ramos, Nino Puma, Víctor Aguilar, Roger Machacca, José Torres, Kevin Cueva, John Cruz, Ivonne Lazarte, Riky Centeno, Rafael Miranda, Yovana Álvarez, Pablo Masias, Javier Vilca, Fredy Apaza, Rolando Chijcheapaza, Javier Calderón, Jesús Cáceres, Jesica Vela. Fecha : Mayo de 2016 Arequipa – Perú Contenido Introducción ...................................................................................................................................... 1 Objetivos ............................................................................................................................................ 3 CAPITULO I ........................................................................................................................................ 4 1. Volcanes Activos en el Sur del Perú ........................................................................................ 4 1.1 Volcán Sabancaya ............................................................................................................. 5 1.2 Misti .................................................................................................................................. -
America's Highest Peak Now Measures 6962 Metres!
America’s highest peak now measures 6962 metres! At 6,962 Metres on Aconcagua in January 2001: Climber Gianpetro Verza has just mounted the terre- strial reflector signal to enable the classical terrestrial survey with tacheometres from the valley, and he has fixed on the top the Leica GPS 530 antenna. This configura- The highest mountain of The 7242 kilometre-long mountains are “growing” tion allowed at the same time mea- the Americas is only 38.17 Andes are the longest or "shrinking". From now on, surement in both technologies with meters short of seven mountain chain in the world. however, with technology high accuracy. Verza has put the thousand. The indications The Swiss Matthias and systems providing a Leica GPS530 terminal, the same on maps of the precise Zurbriggen was the first reproducible accuracy of a equipment as used on Kilimanjaro, elevation of America’s man to conquer Aconcagua few millimetres, it will be before him on the summit. highest peak, Mt Aconca- on 14 January 1897. In 2001 possible to precisely measu- gua, will have to be correc- it was with the most modern re the summits and record re-surveyed using the same ted and increased by two GPS measurement techno- their vertical and horizontal GPS equipment from Leica metres. This is the result of logy from Switzerland, that movements. Geosystems. an Italian-Argentinian the exact mountain height Scientific Expedition led by was re-determined. After Mt Everest and On Mt Everest, re-measured Geologist Giorgio Poretti. Mt Kilimanjaro now also in 1992 by an Italian- Previously -
Archaeological, Radiological, and Biological Evidence Offer Insight Into Inca Child Sacrifice
Archaeological, radiological, and biological evidence offer insight into Inca child sacrifice Andrew S. Wilsona,1, Emma L. Browna, Chiara Villab, Niels Lynnerupb, Andrew Healeyc, Maria Constanza Cerutid, Johan Reinharde, Carlos H. Previglianod,2, Facundo Arias Araozd, Josefina Gonzalez Diezd, and Timothy Taylora,3 aDepartment of Archaeological Sciences, and cCentre for Chemical and Structural Analysis, University of Bradford, Bradford BD7 1DP, United Kingdom; bLaboratory of Biological Anthropology, Department of Forensic Medicine, Faculty of Health Sciences, University of Copenhagen, Blegdamsvej 3, DK-2200 Copenhagen N, Denmark; dInstitute of High Mountain Research, Catholic University of Salta, Salta A4400FYP, Argentina; and eNational Geographic Society, Washington, DC 20036 Edited by Charles Stanish, University of California, Los Angeles, CA, and approved June 18, 2013 (received for review March 21, 2013) Examination of three frozen bodies, a 13-y-old girl and a girl and defining, element of a capacocha ritual. We also recognize that boy aged 4 to 5 y, separately entombed near the Andean summit the capacocha rite analyzed here was embedded within a multi- of Volcán Llullaillaco, Argentina, sheds new light on human sac- dimensional imperial ideology. rifice as a central part of the Imperial Inca capacocha rite, de- The frozen remains of the ∼13-y-old “Llullaillaco Maiden,” the scribed by chroniclers writing after the Spanish conquest. The 4- to 5-y-old “Llullaillaco Boy,” and the 4- to 5-y-old “Lightning high-resolution diachronic data presented here, obtained directly Girl” provide unusual and valuable analytical opportunities. Their from scalp hair, implies escalating coca and alcohol ingestion in the posture and placement within the shrine, surrounded by elite lead-up to death. -
The South American Indian As a Pioneer Alpinist
TI-lE SOUTH AMERICAN INDIAN AS A PIONEER ALPINIST 81 THE SOUTH AMERICAN INDIAN AS A PIONEER ALPINIST BY EVELIO ECHEVARRfA C. ECENTL Y it has become kno\vn that a number of very high Andean mountain tops had not only been ascended but also permanently occupied by the Indians, possibly as much as three centuries before de Saussure's ascent of Mont Blanc. They climbed peaks of up to 22,ooo ft., they constructed shelters on or near their tops, and they used the high places as watch-towers or as sacrificial shrines. Some authorities believe that this activity took place as early as the late four teenth century, though we cannot prove that some of it did not take place long after, possibly as late as the nineteenth century. These Indian accomplishments have been left unmentioned in practi cally all mountaineering history books. In this article, which may be the first to attempt a comprehensive survey,1 my purpose is to review briefly the location and the nature of each discovery. The area in which these Indian mountain ascents took place is what in physical geography is known as the Atacama desert (although this name is nowadays used in political and cultural geography for a much more restricted area). It is a treeless, sandy and volcanic waste-land seldom visited by mountaineers. It stretches from the neighbourhood of Arequipa, in Peru, as far south as Elqui in Chile; to the east it reaches the Andean slopes that face the jungles of Argentina and Bolivia, and to the west, the Pacific Ocean. -
Explora Atacama І Hikes
ATACAMA explorations explora Atacama І Hikes T2 Reserva Tatio T4 Cornisas Nights of acclimatization Nights of acclimatization needed: 2 needed: 0 Type: Half day Type: Half day Duration: 1h Duration: 2h 30 min Distance: 2,3 km / 1,4 mi Distance: 6,7 kms / 4,2 mi Max. Altitude: 4.321 m.a.s.l / Max. Altitude: 2.710 m.a.s.l / HIKES 14.176 f.a.s.l 8.891 f.a.s.l Description: This exploration Description: Departing by van, we offers a different way of visiting head toward the Catarpe Valley Our hikes have been designed according the Tatio geysers, a geothermal by an old road. From there, we to different interests and levels of skill. field with over 80 boiling water hike along the ledges of La Sal They vary in length and difficulty so we sources. In this trip there are Mountains, with panoramic views always recommend travelers to talk to their excellent opportunities of studying of the oasis, the Atacama salt flat, guides before choosing an exploration. the highlands fauna, which includes and The, La Sal, and Domeyko Every evening, guides brief travelers vicuñas, flamingos and foxes, Mountains, three mountain ranges on the different explorations, so that among others. We walk through the that shape the region’s geography. they can choose one that best fit their reserve with views of The Mountains By the end of the exploration we interests. Exploration times do not consider and steaming hot water sources. descend through Marte Valley’s sand transportation. Return to the hotel by van.