Cosmopolitan Highlanders: Region and Nation in Anglo-German
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Atlas of Rare Endemic Vascular Plants of the Arctic
Atlas of Rare Endemic Vascular Plants of the Arctic Technical Report No. 3 About CAFF Theprogram for the Conservation of Arctic Flora and Fauna (CAFF) of the Arctic Council was established lo address the special needs of Arctic ecosystems, species and thcir habitats in the rapid ly developing Arctic region. Itwas initiated as one of'four programs of the Arctic Environmental Protcction Strategy (AEPS) which was adopted by Canada, Denmark/Greenland, Finland, lceland, Norway, Russia, Swcdcn and the United States through a Ministeria! Declaration at Rovaniemi, Finland in 1991. Other programs initi ated under the AEPS and overlaken hy the Are.tie Council are the ArcticMonitoring and assessment Programme (AMAP), the program for Emergency Prevention, Preparcd ness and Response (EPPR) and the program for Protection of the Arctic Marine Envi ronment (PAME). Sinceits inaugural mccti.ng in Ottawa, Canada in 1992, the CAFF program has provided scientists, conscrvation managers and groups, and indigenous people of the north with a distinct forum in which lo tackle a wide range of Arctic conservation issues at the cir cumpolar level. CAFF's main goals, which are achieved in keeping with the concepts of sustainable developrnertt and utilisation, are: • to conserve Arctic Jlora and fauna, thcir diversity and thcir habitats; • to protect the Arctic ecosystems from threats; • to improve conservation management laws, reg ulations and practices for the Arclic; • to integrale Arctic interests into global conservation fora. CAFF operates rhrough a system of Designated Agencies and National Representatives responsible for CAFF in thcir rcspcctivc countries. CAFF also has an International Work ing Group wh.ith has met annually to assess progrcss and to develop Annual WorkPlans. -
Himalaya - Southern-Tibet: the Typical Continent-Continent Collision Orogen
237 Himalaya - Southern-Tibet: the typical continent-continent collision orogen When an oceanic plate is subducted beneath a continental lithosphere, an Andean mountain range develops on the edge of the continent. If the subducting plate also contains some continental lithosphere, plate convergence eventually brings both continents into juxtaposition. While the oceanic lithosphere is relatively dense and sinks into the asthenosphere, the greater sialic content of the continental lithosphere ascribes positive buoyancy in the asthenosphere, which hinders the continental lithosphere to be subducted any great distance. Consequently, a continental lithosphere arriving at a trench will confront the overriding continent. Rapid relative convergence is halted and crustal shortening forms a collision mountain range. The plane marking the locus of collision is a suture, which usually preserves slivers of the oceanic lithosphere that formerly separated the continents, known as ophiolites. The collision between the Indian subcontinent and what is now Tibet began in the Eocene. It involved and still involves north-south convergence throughout southern Tibet and the Himalayas. This youthful mountain area is the type example for studies of continental collision processes. The Himalayas Location The Himalayas form a nearly 3000 km long, 250-350 km wide range between India to the south and the huge Tibetan plateau, with a mean elevation of 5000 m, to the north. The Himalayan mountain belt has a relatively simple, arcuate, and cylindrical geometry over most of its length and terminates at both ends in nearly transverse syntaxes, i.e. areas where orogenic structures turn sharply about a vertical axis. Both syntaxes are named after the main peaks that tower above them, the Namche Barwa (7756 m) to the east and the Nanga Parbat (8138 m) to the west, in Pakistan. -
6.5 Climate Change Projections in the Upper Danube (European Alps) and the Upper Brahmaputra (Himalayas)
6.5 CLIMATE CHANGE PROJECTIONS IN THE UPPER DANUBE (EUROPEAN ALPS) AND THE UPPER BRAHMAPUTRA (HIMALAYAS) Bodo Ahrens∗ and Andreas Dobler IAU, Goethe-University, Frankfurt am Main, Germany 1 INTRODUCTION tion (for further details see Dobler and Ahrens, 2008). In the following sections, statistically Coarse-grid global circulation models (GCMs) downscaled ECHAM5 precipitation fields are do not allow for regional estimates of water bal- named ECHAM5-Γ. They have a grid resolution ◦ ance or trends of extreme precipitation. This is of 0.5 . especially true in complex terrain. Therefore, Trends of daily precipitation statistics are cal- downscaling of the global simulations to gen- culated for all four seasons of the years during erate regional precipitation is necessary. This the simulation period 1960-2080. An overview paper discusses dynamical and statistical down- on the precipitation statistics is provided in Ta- scaling in two major river basins (RBs): (1) the ble 1. The wet day threshold is set to be 1 upper Danube river basin (UDRB) covering an mm/d. Beside the two major RBs, 5 sub-areas area of 76’653 km2 in the European Alps and (2) of interest (see Figs. 1 and 2) are considered. the upper Brahmaputra river basin (UBRB) with The sizes of the single areas (in number of grid ◦ about 500’000 km2 in the Himalayas. The dis- points on the 0.44 simulation grids) are: UDRB cussion focuses on simulated changes of daily 51, Lech RB 5, Salzach RB 7, UBRB 275, As- precipitation statistics in the two RBs. sam 47, Lhasa RB 22 and Wang-Chu RB 8. -
Himalayan Glaciers
Himalayan Glaciers Climate Change, Water Resources, and Water Security Scientific evidence shows that most glaciers in South Asia’s Hindu Kush Himalayan region are retreating, but the consequences for the region’s water supply are unclear, this report finds. The Hindu Kush Himalayan region is the location of several of Asia’s great river systems, which provide water for drinking, irrigation, and other uses for about 1.5 billion people. Recent studies show that at lower elevations, glacial retreat is unlikely to cause significant changes in water availability over the next several decades, but other factors, including groundwater depletion and increasing human water use, could have a greater impact. Higher elevation areas could experience altered water flow in some river basins if current rates of glacial retreat continue, but shifts in the location, intensity, and variability of rain and snow due to climate change will likely have a greater impact on regional water supplies. he Himalayan region, which Tcovers eight countries across Asia, is home to some of the world’s largest and most spectacular glaciers. The melt- water generated from these glaciers each summer supplements the rivers and streams of the region, including several of Asia’s great river systems such as the Indus, Ganges, and Brahmaputra. Rising tempera- tures due to climate change are causing glaciers worldwide to Figure 1. Extending over 2000 kilometers across the Asian continent and including all shrink in volume and or part of Afghanistan, Bangladesh, Bhutan, China, India, Nepal, and Pakistan, the mass, a phenomenon Hindu Kush Himalayan region is the source for many of Asia’s major river systems, known as glacial including the Indus, Ganges, and Brahmaputra. -
24 Portuguese Alpine Club Clube Nacional De Montanhismo CNM
EUMA member (english name) EUMA member (original name) acronym country web page membership member status since 1 Albanian Mountaineering Federation Federata Shqiptare për Alpinizëm dhe Ngjitje FSHALTM Albania http://fshaltm.org/ Full member 2017 2 Alpine Association of Slovenia Planinska zveza Slovenije PZS Slovenia https://www.pzs.si/ Full member 2017 3 Austrian Alpine Club Österreichischer Alpenverein ÖAV/OeAV Austria https://www.alpenverein.at Full member 2017 4 British Mountaineering Council British Mountaineering Council BMC United Kingdom https://www.thebmc.co.uk/ Full member 2017 5 Climbing and Mountaineering Belgium Federation nationale Vereniging zonder winstoogmerk CMBEL Belgium http://cmbel.blogspot.com/ Full member 2017 6 Croatian Mountaineering Association Hrvatski planinarski savez HPS Croatia http://www.hps.hr/ Full member 2017 7 Czech Mountaineering Federation Český horolezecký svaz CHS Czech Republic https://www.horosvaz.cz/ Full member 2017 8 Federation of French Alpine and Mountain Clubs Fédération française des clubs alpins et de montagne FFCAM France https://www.ffcam.fr/ Full member 2017 9 German Alpine Club Deutscher Alpenverein DAV Germany https://www.alpenverein.de/ Full member 2017 10 Hellenic Federation of Mountaineering and Climbing Ελληνική Ομοσπονδία Ορειβασίας – Αναρρίχησης EOOA Greece http://www.eooa.gr/ Full member 2017 11 Italian Alpine Club Club Alpino Italiano CAI Italy http://www.cai.it/ Full member 2017 12 Liechtensteiner Alpine Club Liechtensteiner Alpenverein LAV Liechtenstein http://www.alpenverein.li/ -
Why the Hindu Kush Himalaya Matters
Sustainable Mountain Development RIO 2012 and beyond Why the Hindu Kush Himalaya matters How can the Hindu Kush Himalayas contribute to sustainable development? The HKH mountains abound with diverse natural resources. They provide valuable ecosystem goods and services including water, food, energy, biodiversity, and hydrological regulating functions to support the As the ‘water tower of Asia’, the Hindu Kush Hima- livelihoods of people living upstream and downstream. layan (HKH) mountains are the source of 10 major Mountain ecosystem goods and services support the live- river systems and provide vital ecosystem goods lihoods of more than 210 million mountain inhabitants. and services to more than 1.4 billion people. The region includes four global biodiversity hotspots, Case studies carried out in the HKH suggest that the 488 protected areas, 330 important bird areas, and people of the region can contribute to global sustain- 60 global eco-regions. Rangelands cover more than able development goals by embracing clean energy, 60 per cent of the region’s territory. However the re- community- based management of natural resources, gion is home to more than 40 per cent of the world’s ecotourism, organic farming, and integrated watershed poor people and faces extreme vulnerability and management to enhance and sustain the productivity of risks due to climate and global change. Progressive ecosystem goods and services. However, promotion of warming at higher altitudes has been three to five these solutions requires mountain-focused policies and times the global average; this warming has resulted strategies that take into account mountain specificities – in increased snow and glacial melt and increased fragility, marginality, inaccessibility and adaptability – and frequency of extreme events such as devastating involve the primary stakeholders in deciding priorities and floods and droughts which have exacerbated prob- implementing interventions. -
Quantifying Variability, Source, and Transport of CO in the Urban Areas Over the Himalayas and Tibetan Plateau
Atmos. Chem. Phys., 21, 9201–9222, 2021 https://doi.org/10.5194/acp-21-9201-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Quantifying variability, source, and transport of CO in the urban areas over the Himalayas and Tibetan Plateau Youwen Sun1, Hao Yin1,2, Yuan Cheng3, Qianggong Zhang4,5, Bo Zheng6, Justus Notholt7, Xiao Lu8, Cheng Liu9,2,10,11,1, Yuan Tian12, and Jianguo Liu1 1Key Laboratory of Environmental Optics and Technology, Anhui Institute of Optics and Fine Mechanics, HFIPS, Chinese Academy of Sciences, Hefei 230031, China 2Department of Precision Machinery and Precision Instrumentation, University of Science and Technology of China, Hefei 230026, China 3State Key Laboratory of Urban Water Resource and Environment, School of Environment, Harbin Institute of Technology, Harbin 150090, China 4Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China 5CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing 100101, China 6Institute of Environment and Ecology, Tsinghua Shenzhen International Graduate School, Tsinghua University, Shenzhen 518055, China 7Institute of Environmental Physics, University of Bremen, P.O. Box 330440, 28334 Bremen, Germany 8School of Atmospheric Sciences, Sun Yat-Sen University, Zhuhai 519082, China 9Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China -
An Ascent of the Watzmann Ostwand
An Ascent of the Watzmann Ostwand R ic h a rd N. Me y e r T H E Watzmann, an 8900-foot peak in the Bavarian Alps, domi nates the ancient little town of Berchtesgaden as majestically as the Matterhorn does Zermatt. Many thousands of Americans admire it every year, for Berchtesgaden is a major recreation and vacation center for all the American troops and civilians and their families stationed in Europe. The posh Berchtesgadener Hof, which only a few years ago echoed to the “Heil Hitler” greetings of the Third Reich’s rulers, is now only one of several hotels still under requisi tion by American authorities. There is never a dull moment at Berchtesgaden. Entertainment abounds: all kinds of sports; visits to the bleak, bombed-out resi dences of former Nazi V IP’s; American movies and night clubs; snack bars and real bars. In particular, the American authorities have tried hard to rouse an interest in climbing. The challenge of the peak is always there, an interesting and steep scramble of seven or eight hours with an overnight stay at a comfortable Alpine Club house; and there is a “Watzmann Club” which issues certificates to Amer icans who make the climb. The tour is really worth while, with a fine view and close-ups of magnificent, rugged mountain scenery, not equalled on many a higher and more difficult peak. Despite these well-publicized attractions, the thousands of Amer icans in the valley rarely lift their eyes to the hills. I have been on the Watzmann three times by different routes; and, except my wife and three friends who once accompanied me, I have never seen another American on the mountain or at the cabin. -
Belay Device Recommendation for Single Pitch Climbing
Belay Device Recommendation for Single Pitch Climbing The German Alpine Club (DAV) recommends assisted braking belay devices for belaying single pitch routes in climbing gyms and outdoors. Assisted braking devices offer a safety advantage as compared to manual belay devices. There are different models of assisted braking belay devices on the market. They all have one characteristic in common: In case of a fall they pinch the rope. This is how they assist the belayer’s hand strength. Whether using an assisted braking device or a manual device (e.g. Tube/Munter Hitch): every belay device has specific handling characteristics. Only if you know and are familiar with these characteristics can you belay correctly and avoid errors of application. Qualified training and practice are essential. Crucial issues when belaying with any device: - Always keep a controlling hand on the rope - Practice your device handling before you start belaying - Practice holding falls - Consider the weight difference between climber and belayer - Consider the amount of hand strength required to hold a fall when choosing a device - Choose the right spot for belaying, in particular when the climber is still near the ground - Reduce the amount of slack rope to the utmost, in particular when belaying near the ground - Constantly pay attention What is the advantage of assisted braking belay devices? Especially in gyms and at highly frequented crags, distraction is a serious problem. Inattentiveness may quickly lead to a severe accident. Assisted braking belay devices increase the chance of preventing a fall to the ground despite belaying errors. In particular at artificial climbing walls the route of the rope is often straight so that rope friction is minimal, therefore a large part of the energy of the fall ends up on the belayer. -
The Indian Ocean and the Himalayas : a Geological Interpretation
The Indian Ocean and the Himalayas : a geological interpretation Autor(en): Gansser, Augusto Objekttyp: Article Zeitschrift: Eclogae Geologicae Helvetiae Band (Jahr): 59 (1966) Heft 2 PDF erstellt am: 11.10.2021 Persistenter Link: http://doi.org/10.5169/seals-163396 Nutzungsbedingungen Die ETH-Bibliothek ist Anbieterin der digitalisierten Zeitschriften. Sie besitzt keine Urheberrechte an den Inhalten der Zeitschriften. Die Rechte liegen in der Regel bei den Herausgebern. Die auf der Plattform e-periodica veröffentlichten Dokumente stehen für nicht-kommerzielle Zwecke in Lehre und Forschung sowie für die private Nutzung frei zur Verfügung. Einzelne Dateien oder Ausdrucke aus diesem Angebot können zusammen mit diesen Nutzungsbedingungen und den korrekten Herkunftsbezeichnungen weitergegeben werden. Das Veröffentlichen von Bildern in Print- und Online-Publikationen ist nur mit vorheriger Genehmigung der Rechteinhaber erlaubt. Die systematische Speicherung von Teilen des elektronischen Angebots auf anderen Servern bedarf ebenfalls des schriftlichen Einverständnisses der Rechteinhaber. Haftungsausschluss Alle Angaben erfolgen ohne Gewähr für Vollständigkeit oder Richtigkeit. Es wird keine Haftung übernommen für Schäden durch die Verwendung von Informationen aus diesem Online-Angebot oder durch das Fehlen von Informationen. Dies gilt auch für Inhalte Dritter, die über dieses Angebot zugänglich sind. Ein Dienst der ETH-Bibliothek ETH Zürich, Rämistrasse 101, 8092 Zürich, Schweiz, www.library.ethz.ch http://www.e-periodica.ch The Indian Ocean and the Himalayas A Geological Interpretation by Augusto Gansser (Zürich)1) with 4 figures in the text and 2 plates (I and II) ABSTRACT The recently discovered lineaments of the Indian Ocean indicate a northwards shift of the Indian Shield which is directly responsible for the Himalayan Orogeny. -
THE INDIAN OCEAN the GEOLOGY of ITS BORDERING LANDS and the CONFIGURATION of ITS FLOOR by James F
0 CX) !'f) I a. <( ~ DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY THE INDIAN OCEAN THE GEOLOGY OF ITS BORDERING LANDS AND THE CONFIGURATION OF ITS FLOOR By James F. Pepper and Gail M. Everhart MISCELLANEOUS GEOLOGIC INVESTIGATIONS MAP I-380 0 CX) !'f) PUBLISHED BY THE U. S. GEOLOGICAL SURVEY I - ], WASHINGTON, D. C. a. 1963 <( :E DEPARTMEI'fr OF THE ltfrERIOR TO ACCOMPANY MAP J-S80 UNITED STATES OEOLOOICAL SURVEY THE lliDIAN OCEAN THE GEOLOGY OF ITS BORDERING LANDS AND THE CONFIGURATION OF ITS FLOOR By James F. Pepper and Gail M. Everhart INTRODUCTION The ocean realm, which covers more than 70percent of ancient crustal forces. The patterns of trend of the earth's surface, contains vast areas that have lines or "grain" in the shield areas are closely re scarcely been touched by exploration. The best'known lated to the ancient "ground blocks" of the continent parts of the sea floor lie close to the borders of the and ocean bottoms as outlined by Cloos (1948), who continents, where numerous soundings have been states: "It seems from early geological time the charted as an aid to navigation. Yet, within this part crust has been divided into polygonal fields or blocks of the sea floQr, which constitutes a border zone be of considerable thickness and solidarity and that this tween the toast and the ocean deeps, much more de primary division formed and orientated later move tailed information is needed about the character of ments." the topography and geology. At many places, strati graphic and structural features on the coast extend Block structures of this kind were noted by Krenke! offshore, but their relationships to the rocks of the (1925-38, fig. -
1912 the Mountaineers
The Mountaineer. Volume Five Nineteen Hundred Twelve h611, •• , ,, The Mountaineen Sea11le. Wa1hla1100 :J1'.)1'1zec1 bv G oog I e 2,-�a""" ...._� _..,..i..c.. tyJ Vi) Copyright 1912 The Mountaineers Din,tiZ<'d by Google CONTENTS Page Greeting ................... ................................John Muir .......................................... Greeting ..................................................... Enos Mills ........................................ The Higher Functions of a Mountain Club................................................... \ Wm. Frederic Bade.......................... 9 Little Tahoma ............ ............................. .Edmond S. Meany............................ 13 Mountaineer Outing of 1912 on north side of Mt. Rainier....................... Mary Paschall ................................... 14 Itinerary of Outing of 1912................... .Charles S. Gleason........................... 26 The Ascent of Mt. Rainier.................... £. M.Hack ........................................ 28 Grand Park .............................................. 1=dmond S. Meany............................ 36 A New Route up Mt. Rainier.............. 'Jara Keen ........................................ 37 Naches Pass .............................................. Edmond S. Meany....... ,.................... 40 Undescribed Glaciers of Mt. Rainier .. Fran,ois Matthes ............................. 42 Thermal Caves ....................................... J. B. Flett .......................................... 58 Change in Willis