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  • 1
    Call number: PIK N 454-07-0099
    Type of Medium: Monograph available for loan
    Pages: XIV, 288 p. Karten
    Series Statement: Fluctuations of Glaciers 8
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 2
    Call number: PIK N 454-13-0041
    Type of Medium: Monograph available for loan
    Pages: XIV, 336 S. + 11 Beil.
    Series Statement: Fluctuations of glaciers 10
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    Zürich : Versuchsanst. für Wasserbau, Hydrologie u. Glaziologie an d. Eidgenöss. Techn. Hochsch. Zürich
    Call number: MOP 44721 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 221 S. : Ill., graph. Darst., Kt.
    Series Statement: Mitteilung der Versuchsanstalt für Wasserbau, Hydrologie und Glaziologie an der Eidgenössischen Technischen Hochschule Zürich 17
    Note: Zugl.: Basel, Univ., Diss.
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 4
    Call number: M 20.93497
    Description / Table of Contents: The Himalayas are a region that is most dependent, but also frequently prone to hazards from changing meltwater resources. This mountain belt hosts the highest mountain peaks on earth, has the largest reserve of ice outside the polar regions, and is home to a rapidly growing population in recent decades. One source of hazard has attracted scientific research in particular in the past two decades: glacial lake outburst floods (GLOFs) occurred rarely, but mostly with fatal and catastrophic consequences for downstream communities and infrastructure. Such GLOFs can suddenly release several million cubic meters of water from naturally impounded meltwater lakes. Glacial lakes have grown in number and size by ongoing glacial mass losses in the Himalayas. Theory holds that enhanced meltwater production may increase GLOF frequency, but has never been tested so far. The key challenge to test this notion are the high altitudes of 〉4000 m, at which lakes occur, making field work impractical. Moreover, flood waves can attenuate rapidly in mountain channels downstream, so that many GLOFs have likely gone unnoticed in past decades. Our knowledge on GLOFs is hence likely biased towards larger, destructive cases, which challenges a detailed quantification of their frequency and their response to atmospheric warming. Robustly quantifying the magnitude and frequency of GLOFs is essential for risk assessment and management along mountain rivers, not least to implement their return periods in building design codes. [...]
    Type of Medium: Dissertations
    Pages: 122 Seiten , Illustrationen, Diagramme
    Language: English
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  • 5
    Call number: 8/M 18.91608
    Description / Table of Contents: Snow and Ice-Related Hazards, Risks, and Disasters provides you with the latest scientific developments in glacier surges and melting, ice shelf collapses, paleo-climate reconstruction, sea level rise, climate change implications, causality, impacts, preparedness, and mitigation. It takes a geo-scientific approach to the topic while also covering current thinking about directly related social scientific issues that can adversely affect ecosystems and global economies.Puts the contributions from expert oceanographers, geologists, geophysicists, environmental scientists, and climatologists selec
    Type of Medium: Monograph available for loan
    Pages: xxiv, 762 Seiten , Illustrationen
    ISBN: 978-0-12-394849-6
    Series Statement: Hazards and disasters series
    Classification:
    Natural Disasters, Disaster Management
    Subsequent Title: Snow and ice-related hazards, risks, and disasters (2. Auflage, E-Book (AWI only))
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 6
    Call number: AWI G7-19-92930
    In: Glacier mass balance bulletin, No. 7
    Type of Medium: Series available for loan
    Pages: 87 Seiten , Illustrationen
    Series Statement: Glacier mass balance bulletin 7
    Language: English
    Note: CONTENTS 1. INTRODUCTION 2. SUMMARY DATA 2.1 SUMMARY TABLE (NET BALANCE, ELA, ELA0, AAR, AAR0) 2.2 CUMULATIVE SPECIFIC NET BALANCE GRAPHS 3. EXTENSIVE INFORMATION 3.1 WHITE (CANADA) 3.1.1 Topography and observational network 3.1.2 Net balance maps 1999/2000 and 2000/2001 3.1.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.1.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.2 PEYTO (CANADA) 3.2.1 Topography and observational network 3.2.2 Net balance maps 1999/2000 and 2000/2001 3.2.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.2.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.3 ZONGO (BOLIVIA) 3.3.1 Topography and observational network 3.3.2 Net balance maps 1999/2000 and 2000/2001 3.3.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.3.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.4 WALDEMARBREEN (NORWAY/SVALBARD) 3.4.1 Topography and observational network 3.4.2 Net balance maps 1999/2000 and 2000/2001 3.4.3 Net balance altitude (1999/2000 and 2000/2001) 3.4.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.5 NIGARDSBREEN (NORWAY) 3.5.1 Topography and observational network 3.5.2 Net balance maps 1999/2000 and 2000/2001 3.5.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.5.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.6 STORGLACIÄREN (SWEDEN) 3.6.1 Topography and observational network 3.6.2 Net balance maps 1999/2000 and 2000/2001 3.6.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.6.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.7 VERNAGTFERNER (AUSTRIA) 3.7.1 Topography and observational network 3.7.2 Net balance maps 1999/2000 and 2000/2001 3.7.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.7.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.8 DJANKUAT (RUSSIA) 57 3.8.1 Topography and observational network 3.8.2 Net balance map 2000/2001 3.8.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.8.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.9 TSENTRALNIY TUYUKSUYSKIY (KAZAKHSTAN) 3.9.1 Topography and observational network 3.9.2 Net balance maps 1999/2000 and 2000/2001 3.9.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.9.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.10 MALIYAKTRU (RUSSIA) 3.10.1 Topography and observational network 3.10.2 Net balance maps 1999/2000 and 2000/2001 3.10.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.10.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.11 URUMQIHE S. NO. 1 (CHINA) 3.11.1 Topography and observational network 3.11.2 Net balance maps 1999/2000 and 2000/2001 3.11.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.11.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 4. FINAL REMARKS AND ACKNOWLEDGEMENTS 5. PRINCIPAL INVESTIGATORS AND NATIONAL CORRESPONDENTS 5.1 PRINCIPAL INVESTIGATORS 5.2 NATIONAL CORRESPONDENTS OF WGMS
    Location: AWI Reading room
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  • 7
    Call number: AWI G7-19-92931
    In: Glacier mass balance bulletin, No. 8
    Type of Medium: Series available for loan
    Pages: 100 Seiten , Illustrationen
    Series Statement: Glacier mass balance bulletin 8
    Language: English
    Note: CONTENTS 1 INTRODUCTION 2 BASIC INFORMATION 2.1 SUMMARY TABLE (NET BALANCE, ELA, ELA0, AAR, AAR0) 2.2 CUMULATIVE SPECIFIC NET BALANCE GRAPHS 3 DETAILED INFORMATION 3.1 GLACIAR BAHIA DEL DIABLO (ANTARCTICA) 3.1.1 Topography and observational network 3.1.2 Net balance maps 2001/02 and 2002/03 3.1.3 Net balance versus altitude (2001/02 and 2002/03) 3.1.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.2 MARTIAL ESTE (ARGENTINA) 3.2.1 Topography and observational network 3.2.2 Net balance maps 2001/02 and 2002/03 3.2.3 Net balance versus altitude (2001/02 and 2002/03) 3.2.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.3 VERNAGTFERNER (AUSTRIA) 3.3.1 Topography and observational network 3.3.2 Net balance maps (2001/02 and 2002/03) 3.3.3 Net balance versus altitude (2001/02 and 2002/03) 3.3.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.4 ZONGO (BOLIVIA) 3.4.1 Topography and observational network 3.4.2 Net balance maps (2001/02 and 2002/03) 3.4.3 Net balance versus altitude (2001/02 and 2002/03) 3.4.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.5 WHITE (CANADA) 3.5.1 Topography and observational network 3.5.2 Net balance maps (2001/02 and 2002/03) 3.5.3 Net balance versus altitude (2001/02 and 2002/03) 3.5.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.6 URUMQIHE S. NO. 1 (CHINA) 3.6.1 Topography and observational network 3.6.2 Net balance maps (2001/02 and 2002/03) 3.6.3 Net balance versus altitude (2001/02 and 2002/03) 3.6.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.7 FONTANA BIANCA (ITALY) 3.7.1 Topography and observational network 3.7.2 Net balance maps (2001/02 and 2002/03) 3.7.3 Net balance versus altitude (2001/02 and 2002/03) 3.7.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.8 TSENTRALNIY TUYUKSUYSKIY (KAZAKHSTAN) 3.8.1 Topography and observational network 3.8.2 Net balance map (2001/02 and 2002/03) 3.8.3 Net balance versus altitude (2001/02 and 2002/03) 3.8.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.9 NIGARDSBREEN (NORWAY) 3.9.1 Topography and observational network 3.9.2 Net balance maps (2001/02 and 2002/03) 3.9.3 Net balance versus altitude (2001/02 and 2002/03) 3.9.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.10 WALDEMARBREEN (NORWAY) 3.10.1 Topography and observational network 3.10.2 Net balance maps (2001/02 and 2002/03) 3.10.3 Net balance versus altitude (2001/02 and 2002/03) 3.10.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.11 DJANKUAT (RUSSIA) 3.11.1 Topography and observational network 3.11.2 Net balance maps (2001/02 and 2002/03) 3.11.3 Net balance versus altitude (2001/02 and 2002/03) 3.11.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.12 MALIY AKTRU (RUSSIA) 3.12.1 Topography and observational network 3.12.2 Net balance maps (2001/02 and 2002/03) 3.12.3 Net balance versus altitude (2001/02 and 2002/03) 3.12.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.13 STORGLACIÄREN (SWEDEN) 3.13.1 Topography and observational network 3.13.2 Net balance maps (2001/02 and 2002/03) 3.13.3 Net balance versus altitude (2001/02 and 2002/03) 3.13.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 4 FINAL REMARKS AND ACKNOWLEDGEMENTS 5 PRINCIPAL INVESTIGATORS AND NATIONAL CORRESPONDENTS 5.1 PRINCIPAL INVESTIGATORS 5.2 NATIONAL CORRESPONDENTS OF WGMS
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  • 8
    Call number: 9780128171301 (e-book)
    Type of Medium: 12
    Pages: 1 Online-Ressource (786 Seiten) , Illustrationen
    Edition: 2nd edition
    ISBN: 978-0-12-817130-1
    Series Statement: Hazards and disasters series
    Former Title: Snow and ice-related hazards, risks, and disasters (1. Auflage, Druckausgabe)
    Language: English
    Note: Contents Contributors Editorial foreword Preface CHAPTER 1 Snow and ice-related hazards, risks, and disasters: Facing challenges of rapid change and long-term commitments / Wilfried Haeberli and Colin Whiteman 1.1 Introduction 1.2 Costs and benefits: Living with snow and ice 1.3 Small and large, fast and slow, local to global: Dealing with constraints 1.4 Beyond historical experience: Monitoring, modeling, and managing rapid and irreversible changes Acknowledgments References CHAPTER 2 Physical, thermal, and mechanical properties of snow, ice, and permafrost / Lukas Arenson (U.), William Colgan, and Hans Peter Marshall 2.1 Introduction 2.2 Density and structure 2.2.1 Snow 2.2.2 Ice 2.2.3 Frozen ground/permafrost 2.3 Thermal properties 2.3.1 Snow 2.3.2 Ice 2.3.3 Frozen ground 2.4 Mechanical properties 2.4.1 Brittle behavior 2.4.2 Ductile behavior 2.5 Electromagnetic and wave properties 2.5.1 Snow 2.5.2 Ice 2.5.3 Frozen ground 2.6 Summary Acknowledgment References.. CHAPTER 3 Snow and ice in the climate system / Atsumu Ohmura 3.1 Introduction 3.2 Physical extent of the cryosphere 3.3 Climatic conditions of the cryosphere 3.3.1 Snow cover 3.3.2 Sea ice 3.3.3 Permafrost 3.3.4 Glaciers References CHAPTER 4 Snow and ice in the hydrosphere / Jan Seibert, Michal Jenicek, Matthias Huss, Tracy Ewen, and Daniel Viviroli 4.1 Introduction 4.2 Snow accumulation and melt 4.2.1 Snowpack description 4.2.2 Snow accumulation 4.2.3 Snow redistribution, metamorphism, and ripening process 4.2.4 Snowpack development 4.2.5 Snowmelt 4.3 Glaciers and glacial mass balance 4.3.1 Glacier mass balance 4.3.2 Glacial drainage system 4.3.3 Modeling glacier discharge 4.4 Hydrology of snow- and ice-covered catchments 4.4.1 Influence of snow on discharge 4.4.2 Snowmelt runoff and climate change 4.4.3 Influence of glaciers on discharge 4.4.4 River ice 4.4.5 Seasonally frozen soil and permafrost 4.5 Concluding remarks References CHAPTER 5 Snow, ice, and the biosphere / Terry V. Callaghan and Margareta Johansson 5.1 Introduction 5.2 Adaptations to snow, ice, and permafrost. 5.3 Snow and ice as habitats 5.4 Snow as a moderator of habitat 5.4.1 Modification of winter habitat 5.4.2 Modification of nonwinter habitat 5.4.3 Effects of changing snow on the biosphere 5.5 Ice as a moderator of habitat 5.5.1 Mechanical effects of ice 5.5.2 Effects of changing lake and river ice on the biosphere 5.5.3 Effects of changing sea ice on the biosphere 5.6 Permafrost as a moderator of habitat 5.6.1 Effects of changing permafrost on the biosphere 5.6.2 Snow-permafrost-vegetation interactions 5.7 Vegetation as a moderator of snow, ice, and permafrost habitats 5.8 Conclusions Acknowledgments References CHAPTER 6 Ice and snow as land-forming agents / Darrel A. Swift, Simon Cook, Tobias Heckmann, Isabelle Gärtner-Roer, Oliver Korup, and Jeffrey Moore 6.1 Glacial processes and landscapes 6.1.1 Erosion mechanisms and their controls 6.1.2 Landforms and associated hazards 6.1.3 Landscape evolution and rates of glacial incision 6.1.4 Recommended avenues for further research 6.2 Periglacial and permafrost processes and landforms 6.2.1 Landforms and processes related to seasonal frost and permafrost 6.3 The role of snow in forming landscapes 6.3.1 Influence of snow cover on geomorphic processes 6.3.2 Snow-related geomorphic processes and landforms 6.3.3 Potential impacts of global change on snow-related geomorphic processes 6.3.4 Quantifying rates 6.3.5 Modeling 6.4 Conclusions and outlook Acknowledgments References CHAPTER 7 Mountains, lowlands, and coasts: The physiography of cold landscapes / Tobias Bolch and Hanne H. Christiansen 7.1 Introduction 7.2 Physiography of the terrestrial cryosphere 7.2.1 High altitudes/mountains 7.2.2 Cold lowlands 7.2.3 Cold coasts 7.3 Glaciers and ice sheets: Extent and distribution 7.4 Permafrost types, extent, and distribution 7.5 Glacier-permafrost interactions References CHAPTER 8 A socio-cryospheric systems approach to glacier hazards, glacier runoff variability, and climate change / Mark Carey, Graham McDowell, Christian Huggel, Becca Marshall, Holly Moulton, Cesar Portocarrero, Zachary Provant, John M. Reynolds, and Luis Vicuña 8.1 Introduction 8.2 Integrated adaptation in dynamic socio-cryospheric systems 8.3 Glacier and glacial lake hazards 8.3.1 Cordillera Blanca, Peru 8.3.2 Santa Teresa, Peru 8.3.3 Nepal 8.4 Volcano-ice hazards 8.5 Glacier runoff, hydrologic variability, and water use hazards 8.5.1 Nepal 8.5.2 Peru 8.6 Coastal resources and hazards 8.7 Discussion and conclusions Acknowledgments References CHAPTER 9 Integrative risk management: The example of snow avalanches / Michael Bründl and Stefan Margreth 9.1 Introduction 9.2 Risk analysis 9.2.1 Hazard analysis 9.2.2 Exposure and vulnerability analysis 9.2.3 Consequence analysis and calculation of risk 9.3 Risk evaluation 9.3.1 Evaluation of individual risk 9.3.2 Evaluation of collective risk 9.4 Mitigation of risk 9.4.1 Meaning of mitigation of risk 9.4.2 Technical avalanche mitigation measures 9.4.3 Land-use planning 9.4.4 Biological measures and protection forests 9.4.5 Organizational measures 9.5 Methods and tools for risk assessment and evaluation of mitigation measures 9.6 Case study “Evaluation of avalanche mitigation measures for Juneau, Alaska” 9.6.1 Introduction 9.6.2 Avalanche situation 9.6.3 Hazard analysis 9.6.4 Consequence analysis and risk evaluation 9.6.5 Protection measures 9.6.6 Conclusions 9.7 Final remarks References CHAPTER 10 Permafrost degradation / Dmitry Streletskiy 10.1 Introduction 10.2 Drivers of permafrost and active-layer change across space and time 10.2.1 Role of climate: Air temperature and liquid precipitation 10.2.2 Role of topography 10.2.3 Role of vegetation and snow 10.2.4 Role of soil properties 10.3 Observed permafrost and active-layer changes 10.4 Permafrost modeling and forecasting 10.5 Permafrost degradation and infrastructure hazards 10.5.1 Buildings on permafrost 10.5.2 Pipelines on permafrost 10.5.3 Railroads, roads, and utility on permafrost 10.6 Coastal erosion and permafrost 10.7 Summary Acknowledgments References CHAPTER 11 Radioactive waste under conditions of future ice ages / Urs H. Fischer, Anke Bebiolka, Jenny Brandefelt, Denis Cohen, Joel Harper, Sarah Hirschorn, Mark Jensen, Laura Kennell, Johan Liakka, Jens-Ove Näslund, Stefano Normani, Heidrun Stück, and Axel Weitkamp 11.1 Introduction 11.2 Timing of future glacial inception 11.2.1 Introduction 11.2.2 Definition of glacial inception 11.2.3 Controlling factors of glacial inception 11.2.4 Future long-term variations of insolation and atmospheric greenhouse gas concentrations 11.2.5 Modeling of future glacial inception 11.2.6 Timing of future glacial inception and concluding remarks 11.3 The glacier ice-groundwater interface: Constraints from a transect of the modern Greenland Ice Sheet 11.3.1 Background 11.3.2 Basal thermal state 11.3.3 Framework of the ice-bed interface 11.3.4 Basal water 11.3.5 Summary 11.4 Deep glacial erosion in the Alpine Foreland of northern Switzerland 11.4.1 Background 11.4.2 Ice age conditions 11.4.3 Processes of glacial erosion and glacial overdeepening 11.4.4 Water flow in overdeepenings 11.4.5 Deep glacial erosion in the Swiss Plateau 11.4.6 Future research focus 11.5 Tunnel valleys in Germany and their relevance to the long-term safety of nuclear waste repositories 11.5.1 Background 11.5.2 Formation of tunnel valleys 11.5.3 Tunnel valleys in Northern Germany 11.5.4 Tunnel valleys in the German North Sea 11.5.5 Glacial overdeepening in Southern Germany 11.5.6 Impact of tunnel valley formation on host rocks 11.6 Assessment of glacial impacts on geosphere stability and barrier capacity—Canadian perspective 11.6.1 Background 11.6.2 Bruce Nuclear Site—Location and geologic setting Acknowledgments References CHAPTER 12 Snow avalanches / Jürg Schweizer, Perry Bartelt, and Alec van Herwijnen 12.1 Introduction 12.2 The avalanche phenomenon 12.3 Avalanche release 12.3.1 Dry-snow avalanches 1
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  • 9
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    Unknown
    PANGAEA
    In:  Supplement to: Haeberli, Wilfried; Patzelt, Gernot (1982): Permafrostkartierung im Gebiet der Hochebenkar-Blockgletscher, Obergurgl, Ötztaler Alpen. Zeitschrift für Gletscherkunde und Glazialgeologie, 18(2), 127-150, hdl:10013/epic.40222.d001
    Publication Date: 2023-05-12
    Description: The occurrence of permafrost in the region of the Hochebenkar rock glaciers has been mapped in detail. For this purpose basal temperatures of the winter snow cover were measured at over 250 sites (BTS-method), II refraction-seismic profiles were taken in frozen and unfrozen unconsolidated sediments and 12 springs were investigated in terms of their summer temperature 128 W. Haeberli und G. PatzeIt variations. The combination of seismic refraction and the BTS-method allows rapid and reliable mapping of alpine permafrost, and at the same time enables differences in active-Iayer thickness to be established. The resuIts of the observations confirm the ideas developed in the Swiss Alps in recent years about the relationships between permafrost and rock glaciers: rock glaciers are creep phenomena of discontinuous alpine permafrost.
    Keywords: Geological mapping; GEOMAP; Glaciers Austria; Hochebenkar; Ötztal, Tyrolian Alps, Austria
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 10
    Publication Date: 2023-05-12
    Keywords: Geological mapping; GEOMAP; Glaciers Austria; Hochebenkar; Ötztal, Tyrolian Alps, Austria
    Type: Dataset
    Format: image/jpeg, 9 MBytes
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