Fluctuations of Glaciers 1990-1995 (Vol. VII)

Total Page:16

File Type:pdf, Size:1020Kb

Fluctuations of Glaciers 1990-1995 (Vol. VII) FLUCTUATIONS OF GLACIERS 1990–1995 (Vol. VII) A contribution to the Global Environment Monitoring Service (GEMS) and the International Hydrological Programme (IHP) Prepared by the World Glacier Monitoring Service (WGMS) IAHS (ICSI) – UNEP – UNESCO 1998 FLUCTUATIONS OF GLACIERS 1990–1995 with addendas from earlier years This publication was made possible by support and funds from the Federation of Astronomical and Geophysical Data Analysis Services (FAGS) the Swiss Academy of Sciences (SAS) the University of Zurich (UNIZ) the Federal Institute of Technology (ETH) Zurich This volume continues the earlier works published under the titles FLUCTUATIONS OF GLACIERS 1959–1965 Paris, IAHS – UNESCO, 1967 FLUCTUATIONS OF GLACIERS 1965–1970 Paris, IAHS – UNESCO, 1973 FLUCTUATIONS OF GLACIERS 1970–1975 Paris, IAHS – UNESCO, 1977 FLUCTUATIONS OF GLACIERS 1975–1980 Paris, IAHS – UNESCO, 1985 FLUCTUATIONS OF GLACIERS 1980–1985 Paris, IAHS – UNESCO, 1988 FLUCTUATIONS OF GLACIERS 1985–1990 Paris, IAHS – UNESCO, 1993 FLUCTUATIONS OF GLACIERS 1990–1995 (Vol. VII) A contribution to the Global Environment Monitoring Service (GEMS) and the International Hydrological Programme Compiled for the World Glacier Monitoring Service by Wilfried Haeberli1), Martin Hoelzle1,2), Stephan Suter2) and Regula Frauenfelder1) 1)Department of Geography University of Zurich Zurich and 2)Laboratory of Hydraulics, Hydrology and Glaciology Swiss Federal Institute of Technology (ETH) Zurich International Association of Hydrological Sciences (International Commission on Snow and Ice) and United Nations Environment Programme and United Nations Educational, Scientific and Cultural Organization 1998 Published jointly by the International Association of Hydrological Sciences, IAHS Press, Institute of Hydrology, Wallingford, Oxfordshire 0X10 8BB, UK and the United Nations Environment Programme P.O. Box 30552, Nairobi, Kenya and the United Nations Educational, Scientific and Cultural Organization 7 Place de Fontenoy, 75700 Paris, France Printed by Druckerei Flawil AG Flawil, Switzerland The designations employed and the presentation of the material in this publication do not imply the expression of any opinion what- soever on the part of the publishers concerning the legal status of any country or territory, or of its authorities, or concerning the frontiers of any country or territory. For bibliographic and reference purposes this publication should be referred to as: IAHS/UNESCO (1998). Fluctuations of Glaciers 1990–1995. Volume VII, Zurich: World Glacier Monitoring Service. IAHS UNEP UNESCO PREFACE Following the recent Second IPCC Assessment, there has been an escalation in publicity concerning the potential impacts of climate variability and change on the environment. Particular attention has been given to the consequences of climate change on society, especially within the framework of socio-economies. A fundamental societal need is an abundant supply of high quality water. It is now acknowledged within international circles that ‘water’ will be the critical issue of the 21st century, due to various socio- economic pressures arising from the global increase in population. The prospect of climate variability and change will only enhance further pressures on the diminishing, potable water resources. Thus it is critical to water resources management to have the necessary instruments for predicting and detecting climate change. Monitoring of the changes in glacier mass balances provides a very sensitive detector of natural and anthropogenic-induced climate variability which complement predictions from General Circulation Models (GCMs). Should significant climate change take place in the long term, the resulting glacier fluctuations will have major impacts both on river regimes downstream and on water resources management. Such aspects are of particular relevance to the continued implementation of the Fifth Phase of UNESCO’s Interna- tional Hydrological Programme. Consequently, the publication of Volume VII, 1990–1995, within the Fluctuation of Glaciers series is a timely contribution to the climate change issue. Furthermore this work complements the recent publication of the UNESCO Studies & Reports in Hydrology Series no. 57, entitled Into the 2nd Century of World Glacier Monitoring: Prospects and Strategies, and the earlier release of Glacier Mass Balance Bulletin No. 4 (1994–1995). All these publications have been in co-ordi- nation with the International Commission on Snow and Ice (ICSI) which assists the IHP-V with the implementation of project 1.3, “Hydrological interpretation of global change predictions”. The present Fluctuation of Glaciers volume is also a significant contribution towards The Second International Conference on Climate and Water, Espoo, Finland, August 1998. There are several important messages to the climate change communit found in this vol- ume. Foremost is that mass balances from 33 glaciers reflects continued glacier melting at an accelerated rate. The mean specific net balance (-287 mm) of the corresponding ref- erence glaciers for the five years 1990/91–1994/95 corresponds to an additional energy flux (2–3 Wm-2). It is considered that this flux corresponds to the estimated an- thropogenic greenhouse forcing and is slightly higher than the decadal mean of 1980–1990 (-277 mm). These means are, however, strongly influenced by the bias in geo- graphic-weighting towards Alpine and Scandinavian glaciers within the basic network. In that regard, it is appropriate to highlight the recent ICSI initiative in organizing a sym- posium on Glaciers in the Southern Hemisphere, Melbourne, July 1997, and a corre- sponding monograph which will be published shortly. Especially pertinent, the contents of the present book also remind us that natural climate variability is also capable of producing dramatic changes when concerning the European alpine glaciers, there was a near 50% reduction in total glacier volume from 1850 to the mid-1970s. Most of this change took place during the second half of the 19th century and the first half of the 20th century during times of relatively weak anthropogenic forcing. Filtering the effects of I natural climate variability from those attributed to anthropogenic influences poses one of the principal challenges to the global change scientific community. The World Glacier Monitoring Service is once again to be congratulated for continuing its efforts in producing this seventh volume in the Fluctuation of Glaciers series under the guidance and persistent efforts of Wilfried Haeberli and his collaborators. M. Bonell Chief, Section on Hydrological Processes & Climate International Hydrological Programme, UNESCO II FOREWORD Volume VII of the series of publications on the Fluctuations of Glaciers prepared by the World Glacier Monitoring Service covers a period of unprecedented interest in the mass balance of glaciers. As the general public wake up to the possibility of significant anthropogenic climate change within decades, they have realized that small glaciers are sensitive indicators of present climatic trends. The wasting away of the local glacier brings home the impact of climate warming to many non-scientists in a very vivid way. They want to know more – as do the world leaders who have to make difficult decisions balancing economic and environmental considerations . The information gathered for this publication allows scientists to give a balanced report of the health of glaciers world-wide. Those we know about are melting at an accelerating rate (except in parts of Scandinavia) and their meltwater makes an ever-greater contribu- tion to sea-level rise. However, there are many parts of the world where far too few gla- ciers are monitored. Over the last five years glaciologists have developed improved meth- ods of deducing the mass balance of unmeasured glaciers, often using data provided by the WGMS to test and improve their modelling techniques. In this way the predictions of the effects of climate change on glaciers world-wide are improved. The WGMS is to be congratulated on the production of this volume, which makes data from all over the world available to the glaciological community. The printed maps and tables complement data held in electronic form which, we must remember, is not always easily accessible for some researchers. Above all the efforts of the WGMS to ensure that valuable data are collected centrally has a stimulating effect on the community and en- courages the field scientist to continue with the important, but sometimes lonely task of collecting glacier fluctuation data. The work of the WGMS continues the long tradition of glacier monitoring which began in 1894. It is supported enthusiastically by ICSI (The International Commission on Snow and Ice) and we congratulate Professor Haeberli on bringing another volume in the valu- able Fluctuations of Glaciers series to publication. M. Kuhn E. M. Morris President, ICSI 1991–1995 President, ICSI 1995–2001 III IV PRELIMINARY REMARKS AND THANKS The present Volume VII of the “Fluctuations of Glaciers” mainly concerns the time peri- od from 1990 to 1995. It was prepared by the World Glacier Monitoring Service (WGMS) and continues the corresponding series of publications which contain internationally collected, standardized data on current changes in glaciers throughout the world, i.e.: Vol. I : Fluctuations of Glaciers 1959–1965 (P. Kasser) Vol. II : Fluctuations of Glaciers 1965–1970 (P. Kasser) Vol. III : Fluctuations of Glaciers 1970–1975 (F. Müller) Vol. IV
Recommended publications
  • University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY of the SCOTT GLACIER and WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA
    This dissertation has been /»OOAOO m icrofilm ed exactly as received MINSHEW, Jr., Velon Haywood, 1939- GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA. The Ohio State University, Ph.D., 1967 Geology University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University by Velon Haywood Minshew, Jr. B.S., M.S, The Ohio State University 1967 Approved by -Adviser Department of Geology ACKNOWLEDGMENTS This report covers two field seasons in the central Trans- antarctic Mountains, During this time, the Mt, Weaver field party consisted of: George Doumani, leader and paleontologist; Larry Lackey, field assistant; Courtney Skinner, field assistant. The Wisconsin Range party was composed of: Gunter Faure, leader and geochronologist; John Mercer, glacial geologist; John Murtaugh, igneous petrclogist; James Teller, field assistant; Courtney Skinner, field assistant; Harry Gair, visiting strati- grapher. The author served as a stratigrapher with both expedi­ tions . Various members of the staff of the Department of Geology, The Ohio State University, as well as some specialists from the outside were consulted in the laboratory studies for the pre­ paration of this report. Dr. George E. Moore supervised the petrographic work and critically reviewed the manuscript. Dr. J. M. Schopf examined the coal and plant fossils, and provided information concerning their age and environmental significance. Drs. Richard P. Goldthwait and Colin B. B. Bull spent time with the author discussing the late Paleozoic glacial deposits, and reviewed portions of the manuscript.
    [Show full text]
  • Analogue Sites for Mars Missions: MSL and Beyond
    Program and Abstract Volume LPI Contribution No. 1612 Analogue Sites for Mars Missions: MSL and Beyond March 5–6, 2011 • The Woodlands, Texas Sponsors National Aeronautics and Space Administration Lunar and Planetary Institute Conveners Mary Voytek, NASA Headquarters Michael Meyer, NASA Headquarters Victoria Hipkin, Canadian Space Agency Richard Leveille, Canadian Space Agency Shawn Domagal-Goldman, NASA Headquarters Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 LPI Contribution No. 1612 Compiled in 2011 by Meeting and Publication Services Lunar and Planetary Institute USRA Houston 3600 Bay Area Boulevard, Houston TX 77058-1113 The Lunar and Planetary Institute is operated by the Universities Space Research Association under a cooperative agreement with the Science Mission Directorate of the National Aeronautics and Space Administration. Any opinions, findings, and conclusions or recommendations expressed in this volume are those of the author(s) and do not necessarily reflect the views of the National Aeronautics and Space Administration. Material in this volume may be copied without restraint for library, abstract service, education, or personal research purposes; however, republication of any paper or portion thereof requires the written permission of the authors as well as the appropriate acknowledgment of this publication. Abstracts in this volume may be cited as Author A. B. (2011) Title of abstract. In Analogue Sites for Mars Missions: MSL and Beyond, p. XX. LPI Contribution No. 1612, Lunar and Planetary Institute, Houston. ISSN No. 0161-5297 Preface This volume contains abstracts that have been accepted for presentation at the workshop on Analogue Sites for Mars Missions: MSL and Beyond, March 5–6, 2011, The Woodlands, Texas.
    [Show full text]
  • Modelling the Transfer of Supraglacial Meltwater to the Bed of Leverett Glacier, Southwest Greenland
    The Cryosphere, 9, 123–138, 2015 www.the-cryosphere.net/9/123/2015/ doi:10.5194/tc-9-123-2015 © Author(s) 2015. CC Attribution 3.0 License. Modelling the transfer of supraglacial meltwater to the bed of Leverett Glacier, Southwest Greenland C. C. Clason1, D. W. F. Mair2, P. W. Nienow3, I. D. Bartholomew3, A. Sole4, S. Palmer5, and W. Schwanghart6 1Department of Physical Geography and Quaternary Geology, Stockholm University, 106 91 Stockholm, Sweden 2Geography and Environment, University of Aberdeen, Aberdeen, AB24 3UF, UK 3School of Geosciences, University of Edinburgh, Edinburgh, EH8 9XP, UK 4Department of Geography, University of Sheffield, Sheffield, S10 2TN, UK 5Geography, College of Life and Environmental Sciences, University of Exeter, Exeter, EX4 4RJ, UK 6Institute of Earth and Environmental Science, University of Potsdam, 14476 Potsdam-Golm, Germany Correspondence to: C. C. Clason ([email protected]) Received: 23 June 2014 – Published in The Cryosphere Discuss.: 29 July 2014 Revised: 12 December 2014 – Accepted: 24 December 2014 – Published: 22 January 2015 Abstract. Meltwater delivered to the bed of the Greenland melt to the bed matches the observed delay between the peak Ice Sheet is a driver of variable ice-motion through changes air temperatures and subsequent velocity speed-ups, while in effective pressure and enhanced basal lubrication. Ice sur- the instantaneous transfer of melt to the bed in a control sim- face velocities have been shown to respond rapidly both ulation does not. Although both moulins and lake drainages to meltwater production at the surface and to drainage of are predicted to increase in number for future warmer climate supraglacial lakes, suggesting efficient transfer of meltwa- scenarios, the lake drainages play an increasingly important ter from the supraglacial to subglacial hydrological systems.
    [Show full text]
  • Martian Crater Morphology
    ANALYSIS OF THE DEPTH-DIAMETER RELATIONSHIP OF MARTIAN CRATERS A Capstone Experience Thesis Presented by Jared Howenstine Completion Date: May 2006 Approved By: Professor M. Darby Dyar, Astronomy Professor Christopher Condit, Geology Professor Judith Young, Astronomy Abstract Title: Analysis of the Depth-Diameter Relationship of Martian Craters Author: Jared Howenstine, Astronomy Approved By: Judith Young, Astronomy Approved By: M. Darby Dyar, Astronomy Approved By: Christopher Condit, Geology CE Type: Departmental Honors Project Using a gridded version of maritan topography with the computer program Gridview, this project studied the depth-diameter relationship of martian impact craters. The work encompasses 361 profiles of impacts with diameters larger than 15 kilometers and is a continuation of work that was started at the Lunar and Planetary Institute in Houston, Texas under the guidance of Dr. Walter S. Keifer. Using the most ‘pristine,’ or deepest craters in the data a depth-diameter relationship was determined: d = 0.610D 0.327 , where d is the depth of the crater and D is the diameter of the crater, both in kilometers. This relationship can then be used to estimate the theoretical depth of any impact radius, and therefore can be used to estimate the pristine shape of the crater. With a depth-diameter ratio for a particular crater, the measured depth can then be compared to this theoretical value and an estimate of the amount of material within the crater, or fill, can then be calculated. The data includes 140 named impact craters, 3 basins, and 218 other impacts. The named data encompasses all named impact structures of greater than 100 kilometers in diameter.
    [Show full text]
  • Program and Abstracts of 2017 Congress / Programme Et Résumés
    1 Sponsors | Commanditaires Gold Sponsors | Commanditaires d’or Silver Sponsors | Commanditaires d’argent Other Sponsors | Les autres Commanditaires 2 Contents Sponsors | Commanditaires .......................................................................................................................... 2 Welcome from the Premier of Ontario .......................................................................................................... 5 Bienvenue du premier ministre de l'Ontario .................................................................................................. 6 Welcome from the Mayor of Toronto ............................................................................................................ 7 Mot de bienvenue du maire de Toronto ........................................................................................................ 8 Welcome from the Minister of Fisheries, Oceans and the Canadian Coast Guard ...................................... 9 Mot de bienvenue de ministre des Pêches, des Océans et de la Garde côtière canadienne .................... 10 Welcome from the Minister of Environment and Climate Change .............................................................. 11 Mot de bienvenue du Ministre d’Environnement et Changement climatique Canada ................................ 12 Welcome from the President of the Canadian Meteorological and Oceanographic Society ...................... 13 Mot de bienvenue du président de la Société canadienne de météorologie et d’océanographie .............
    [Show full text]
  • Variations of Patagonian Glaciers, South America, Utilizing RADARSAT Images
    Variations of Patagonian Glaciers, South America, utilizing RADARSAT Images Masamu Aniya Institute of Geoscience, University of Tsukuba, Ibaraki, 305-8571 Japan Phone: +81-298-53-4309, Fax: +81-298-53-4746, e-mail: [email protected] Renji Naruse Institute of Low Temperature Sciences, Hokkaido University, Sapporo, 060-0819 Japan, Phone: +81-11-706-5486, Fax: +81-11-706-7142, e-mail: [email protected] Gino Casassa Institute of Patagonia, University of Magallanes, Avenida Bulness 01855, Casilla 113-D, Punta Arenas, Chile, Phone: +56-61-207179, Fax: +56-61-219276, e-mail: [email protected] and Andres Rivera Department of Geography, University of Chile, Marcoleta 250, Casilla 338, Santiago, Chile, Phone: +56-2-6783032, Fax: +56-2-2229522, e-mail: [email protected] Abstract Combining RADARSAT images (1997) with either Landsat MSS (1987 for NPI) or TM (1986 for SPI), variations of major glaciers of the Northern Patagonia Icefield (NPI, 4200 km2) and of the Southern Patagonia Icefield (SPI, 13,000 km2) were studied. Of the five NPI glaciers studied, San Rafael Glacier showed a net advance, while other glaciers, San Quintin, Steffen, Colonia and Nef retreated during the same period. With additional data of JERS-1 images (1994), different patterns of variations for periods of 1986-94 and 1994-97 are recognized. Of the seven SPI glaciers studied, Pio XI Glacier, the largest in South America, showed a net advance, gaining a total area of 5.66 km2. Two RADARSAT images taken in January and April 1997 revealed a surge-like very rapid glacier advance.
    [Show full text]
  • A Hydrographic Approach to the Alps
    • • 330 A HYDROGRAPHIC APPROACH TO THE ALPS A HYDROGRAPHIC APPROACH TO THE ALPS • • • PART III BY E. CODDINGTON SUB-SYSTEMS OF (ADRIATIC .W. NORTH SEA] BASIC SYSTEM ' • HIS is the only Basic System whose watershed does not penetrate beyond the Alps, so it is immaterial whether it be traced·from W. to E. as [Adriatic .w. North Sea], or from E. toW. as [North Sea . w. Adriatic]. The Basic Watershed, which also answers to the title [Po ~ w. Rhine], is short arid for purposes of practical convenience scarcely requires subdivision, but the distinction between the Aar basin (actually Reuss, and Limmat) and that of the Rhine itself, is of too great significance to be overlooked, to say nothing of the magnitude and importance of the Major Branch System involved. This gives two Basic Sections of very unequal dimensions, but the ., Alps being of natural origin cannot be expected to fall into more or less equal com­ partments. Two rather less unbalanced sections could be obtained by differentiating Ticino.- and Adda-drainage on the Po-side, but this would exhibit both hydrographic and Alpine inferiority. (1) BASIC SECTION SYSTEM (Po .W. AAR]. This System happens to be synonymous with (Po .w. Reuss] and with [Ticino .w. Reuss]. · The Watershed From .Wyttenwasserstock (E) the Basic Watershed runs generally E.N.E. to the Hiihnerstock, Passo Cavanna, Pizzo Luceridro, St. Gotthard Pass, and Pizzo Centrale; thence S.E. to the Giubing and Unteralp Pass, and finally E.N.E., to end in the otherwise not very notable Piz Alv .1 Offshoot in the Po ( Ticino) basin A spur runs W.S.W.
    [Show full text]
  • Caverns Measureless to Man: Interdisciplinary Planetary Science & Technology Analog Research Underwater Laser Scanner Survey (Quintana Roo, Mexico)
    Caverns Measureless to Man: Interdisciplinary Planetary Science & Technology Analog Research Underwater Laser Scanner Survey (Quintana Roo, Mexico) by Stephen Alexander Daire A Thesis Presented to the Faculty of the USC Graduate School University of Southern California In Partial Fulfillment of the Requirements for the Degree Master of Science (Geographic Information Science and Technology) May 2019 Copyright © 2019 by Stephen Daire “History is just a 25,000-year dash from the trees to the starship; and while it’s going on its wild and woolly but it’s only like that, and then you’re in the starship.” – Terence McKenna. Table of Contents List of Figures ................................................................................................................................ iv List of Tables ................................................................................................................................. xi Acknowledgements ....................................................................................................................... xii List of Abbreviations ................................................................................................................... xiii Abstract ........................................................................................................................................ xvi Chapter 1 Planetary Sciences, Cave Survey, & Human Evolution................................................. 1 1.1. Topic & Area of Interest: Exploration & Survey ....................................................................12
    [Show full text]
  • Project ICEFLOW
    ICEFLOW: short-term movements in the Cryosphere Bas Altena Department of Geosciences, University of Oslo. now at: Institute for Marine and Atmospheric research, Utrecht University. Bas Altena, project Iceflow geometric properties from optical remote sensing Bas Altena, project Iceflow Sentinel-2 Fast flow through icefall [published] Ensemble matching of repeat satellite images applied to measure fast-changing ice flow, verified with mountain climber trajectories on Khumbu icefall, Mount Everest. Journal of Glaciology. [outreach] see also ESA Sentinel Online: Copernicus Sentinel-2 monitors glacier icefall, helping climbers ascend Mount Everest Bas Altena, project Iceflow Sentinel-2 Fast flow through icefall 0 1 2 km glacier surface speed [meter/day] Khumbu Glacier 0.2 0.4 0.6 0.8 1.0 1.2 Mt. Everest 300 1800 1200 600 0 2/4 right 0 5/4 4/4 left 4/4 2/4 R 3/4 L -300 terrain slope [deg] Nuptse surface velocity contours Western Chm interval per 1/4 [meter/day] 10◦ 20◦ 30◦ 40◦ [outreach] see also Adventure Mountain: Mount Everest: The way the Khumbu Icefall flows Bas Altena, project Iceflow Sentinel-2 Fast flow through icefall ∆H Ut=2000 U t=2020 H internal velocity profile icefall α 2A @H 3 U = − 3+2 H tan αρgH @x MSc thesis research at Wageningen University Bas Altena, project Iceflow Quantifying precision in velocity products 557 200 557 600 7 666 200 NCC 7 666 000 score 1 7 665 800 Θ 0.5 0 7 665 600 557 460 557 480 557 500 557 520 7 665 800 search space zoom in template/chip correlation surface 7 666 200 7 666 200 7 666 000 7 666 000 7 665 800 7 665 800 7 665 600 7 665 600 557 200 557 600 557 200 557 600 [submitted] Dispersion estimation of remotely sensed glacier displacements for better error propagation.
    [Show full text]
  • Tours and Activities Season 2020-2021
    Tours and Activities Season 2020-2021 Activities at Other activities Activities at EOLO Los Glaciares National Park in the area Tours and Activities Through the following guide, we expose the most representative activities in the area, in order to explore the surroundings of EOLO and Los Glaciares National Park. At EOLO, we can help you design the program that best suits your preferences, physical condition and duration of the stay, thus achieving an optimal itinerary to discover southern Patagonia and all its attractions. General notes . All activities are subject to availability, which is why we suggest booking in advance. Being outdoor activities, weather conditions could cause possible cancellations, changes or adjustments on the itinerary. The activities that take place in the National Park are conducted by companies designated by the National Park Administration. How to use the tours and activities guide: . The activities are grouped according to four main areas: Activities at EOLO, Perito Moreno Glacier area, Punta Bandera Port area, Other activities. We recommend to engage in one activity per area. It is required to hire a shuttle and an authorized guide to access the Perito Moreno glacier area. Both services are booked separately from the tours. To access Punta Bandera port area, it is also required to hire a shuttle, booked separately from the tours. El Chaltén Lago Vie dm a Upsala Glacier CHILE Estancia Cristina Spegazzini Glacier Lago Argentino Airport Punta Bandera El Calafate EOLO Perito Moreno Glacier Roca Lake 20 km 10 ml Google Activities at EOLO The land where the hotel stands extends to 10.000 acres, 30 minutes away from El Calafate, TREKKING on the way to Perito Moreno glacier.
    [Show full text]
  • Alpine Adventures 2019 68
    RYDER WALKER THE GLOBAL TREKKING SPECIALISTS ALPINE ADVENTURES 2019 68 50 RYDER WALKER ALPINE ADVENTURES CONTENTS 70 Be the first to know. Scan this code, or text HIKING to 22828 and receive our e-newsletter. We’ll send you special offers, new trip info, RW happenings and more. 2 RYDERWALKER.COM | 888.586.8365 CONTENTS 4 Celebrating 35 years of Outdoor Adventure 5 Meet Our Team 6 Change and the Elephant in the Room 8 Why Hiking is Important – Watching Nature 10 Choosing the Right Trip for You 11 RW Guide to Selecting Your Next Adventure 12 Inspired Cuisine 13 First Class Accommodations 14 Taking a Closer Look at Huts 15 Five Reasons Why You Should Book a Guided Trek 16 Self-Guided Travel 17 Guided Travel & Private Guided Travel EASY TO MODERATE HIKING 18 Highlights of Switzerland: Engadine, Lago Maggiore, Zermatt 20 England: The Cotswolds 22 Isola di Capri: The Jewel of Southern Italy NEW 24 French Alps, Tarentaise Mountains: Bourg Saint Maurice, Sainte Foy, Val d’Isère 26 Sedona, Arches & Canyonlands 28 Croatia: The Dalmatian Coast 28 30 Engadine Trek 32 Scotland: Rob Roy Way 34 Montenegro: From the Durmitor Mountain Range to the Bay of Kotor 36 New Mexico: Land of Enchantment, Santa Fe to Taos NEW 38 Slovakia: Discover the Remote High Tatras Mountains NEW MODERATE TO CHALLENGING HIKING 40 Heart of Austria 42 Italian Dolomites Trek 44 High Peaks of the Bavarian Tyrol NEW 46 Sicily: The Aeolian Islands 48 Rocky Mountain High Life: Aspen to Telluride 50 New Brunswick, Canada: Bay of Fundy 52 Via Ladinia: Italian Dolomites 54 Dolomiti di
    [Show full text]
  • Korean Direct
    AAC Publications Korean Direct The First Ascent Of Gasherbrum V Insignificant against the blinding white backdrop of Gasherbrum V’s south face, we stood like silhouettes atop a moraine, the wall before us in full view. The complex glacier leading up to the face reminded me of scaly dragon’s tail. We had spotted a snaking line that would lead us to the jagged bergschrund at the foot of the wall. Once on the face, we would have to keep left to avoid a menacing serac, then move right in the upper mixed section before finishing with a direct line to the top. Seong Nak-jong and I had never really considered a route on the south side of unclimbed Gasherbrum V until we were denied passage up the northeast face. We had started our first attempt on the 7,147- meter peak from Camp 1 on the South Gasherbrum Glacier, along the normal routes to Gasherbrums I and II. We trudged through thigh-deep snow to reach the northeast face, which was covered in loose ice and snow, and was nearly impossible to protect. Falling ice and spindrift poured down from above. We finally had no choice but to evacuate from our high point of 6,400 meters. This unsuccessful attempt quashed our desire to climb. As the leader of our small team, the quandaries of a second attempt weighed heavily on my mind. Not only were we physically weakened and our confidence shot, it was already mid-July and more snow was laying siege to the camps. We had been away from home for more than a month.
    [Show full text]