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9 - Glacier- and permafrost-related slope instabilities

from Part II - Processes

Published online by Cambridge University Press:  05 September 2015

Christian Huggel
Affiliation:
Universität Zürich
Mark Carey
Affiliation:
University of Oregon
John J. Clague
Affiliation:
Simon Fraser University, British Columbia
Andreas Kääb
Affiliation:
Universitetet i Oslo
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The High-Mountain Cryosphere
Environmental Changes and Human Risks
, pp. 147 - 165
Publisher: Cambridge University Press
Print publication year: 2015

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References

Barsch, D, Fierz, H, Haeberli, W. Shallow core drilling and bore-hole measurements in the permafrost of an active rock glacier near the Grubengletscher, Wallis, Swiss Alps. Arctic and Alpine Research. 1979;11(2):215228.CrossRefGoogle Scholar
French, H, Thorn, CE. The changing nature of periglacial geomorphology. Géomorphologie: Relief, Processus, Environnement. 2006;3:113.Google Scholar
NRC-Permafrost-Subcommitee. Glossary of permafrost and related ground-ice terms. NRC Technical Memorandum. 1988;142:1156.Google Scholar
Lock, GSH. The Growth and Decay of Ice. Cambridge: Cambridge University Press; 2005.Google Scholar
Jaeger, C. Rock Mechanics and Engineering. Cambridge: Cambridge University Press; 2009.Google Scholar
Etzelmüller, B, Hagen, JO. Glacier–permafrost interactions in Arctic and alpine mountain environments with examples from southern Norway and Svalbard. In: Harris, C, Murton, JB (eds) Cryospheric Systems: Glaciers and Permafrost. London: Geological Society Special Publication; 2005. pp. 1127.Google Scholar
Fischer, L, Huggel, C, Kaab, A, Haeberli, W. Slope failures and erosion rates on a glacierized high-mountain face under climatic changes. Earth Surface Processes and Landforms. 2013;38(8):836846.CrossRefGoogle Scholar
Haeberli, W. Investigating glacier–permafrost relationships in high-mountain area: historical background, selected examples and research needs. In: Harris, C, Murton, JB (eds) Cryospheric Systems: Glaciers and Permafrost. London: Geological Society Special Publication; 2005. pp. 2937.Google Scholar
Gruber, S, Hoelzle, M, Haeberli, W. Permafrost thaw and destabilization of Alpine rock walls in the hot summer of 2003. Geophysical Research Letters. 2004;31(13):L15054.CrossRefGoogle Scholar
Huggel, C. Recent extreme slope failures in glacial environments: effects of thermal perturbation. Quaternary Science Reviews. 2009;28(11–12):11191130.CrossRefGoogle Scholar
Wegmann, M, Gudmundsson, GH, Haeberli, W. Permafrost changes in rock walls and the retreat of Alpine glaciers: a thermal modelling approach. Permafrost and Periglac Process. 1998;9:2333.3.0.CO;2-Y>CrossRefGoogle Scholar
Moorman, BJ. Glacier–permafrost hydrological interconnectivity: Stagnation Glacier, Bylot Island, Canada. In: Harris, C, Murton, JB (eds) Cryospheric Systems: Glaciers and Permafrost. London: Geological Society Special Publication; 2005. pp. 6374.Google Scholar
Hasler, A, Gruber, S, Font, M, Dubois, M. Advective heat transport in frozen rock clefts: conceptual model. Permafrost and Periglacial Processes. 2011; 22(4):378389.CrossRefGoogle Scholar
Gruber, S, Hoelzle, M, Haeberli, W. Rock-wall temperatures in the Alps: modelling their topographic distribution and regional differences. Permafrost and Periglacial Processes. 2004;15(3):299307.CrossRefGoogle Scholar
Hoelzle, M, Mittaz, C, Etzelmüller, B, Haeberli, W. Surface energy fluxes and distribution models of permafrost in European mountain areas: an overview of current developments. Permafrost and Periglacial Processes. 2001;12(1):5368.CrossRefGoogle Scholar
Noetzli, J, Gruber, S. Transient thermal effects in Alpine permafrost. The Cryosphere. 2009;3:8599.CrossRefGoogle Scholar
Kohl, T. Transient thermal effects below complex topographies. Tectonophysics. 1999;306(3–4):311324.CrossRefGoogle Scholar
Noetzli, J. Modeling transient three-dimensional temperature fields in mountain permafrost. PhD. University of Zurich; 2008.Google Scholar
Kukkonen, IT, Safanda, J. Numerical modelling of permafrost in bedrock in northern Fennoscandia during the Holocene. Global Planetary Change. 2001;29:259274.CrossRefGoogle Scholar
Nogués-Bravo, D, Araújo, MB, Errea, MP, Martínez-Rica, JP. Exposure of global mountain systems to climate warming during the 21st century. Global Environmental Change. 2007;17:420428.CrossRefGoogle Scholar
Krautblatter, M, Huggel, C, Deline, P, Hasler, A. Research perspectives on unstable high-alpine bedrock permafrost: measurement, modelling and process understanding. Permafrost and Periglacial Processes. 2012;23(1):8088.CrossRefGoogle Scholar
Huggel, C, Clague, JJ, Korup, O. Is climate change responsible for changing landslide activity in high mountains? Earth Surface Processes and Landforms. 2012;37(1):7791.CrossRefGoogle Scholar
Ravanel, L, Deline, P. Climate influence on rockfalls in high-Alpine steep rockwalls: the north side of the Aiguilles de Chamonix (Mont Blanc massif) since the end of the Little Ice Age. Holocene. 2011;21:357365.CrossRefGoogle Scholar
Davies, MCR, Hamza, O, Harris, C. The effect of rise in mean annual temperature on the stability of rock slopes containing ice-filled discontinuities. Permafrost and Periglacial Processes. 2001;12(1):137144.CrossRefGoogle Scholar
Krautblatter, M, Funk, D, Guenzel, F. Why permafrost rocks become unstable: a rock–ice-mechanical model in time and space. Earth Surface Processes and Landforms. 2013;38(8):876887.CrossRefGoogle Scholar
Mellor, M (ed.). Mechanical Properties of Rocks at Low Temperatures. 2nd Int Conference on Permafrost; 1973; Yakutsk, Russia.Google Scholar
Pudasaini, SP, Krautblatter, M. A two-phase mechanical model for rock-ice avalanches. Journal of Geophysical Research: Earth Surface. 2014;119(10):22722290.CrossRefGoogle Scholar
Sass, O. Spatial patterns of rockfall intensity in the northern Alps. Zeitschrift für Geomorphologie. 2005; 138:5165.Google Scholar
Krautblatter, M, Moore, JR. Rock slope instability and erosion: toward improved process understanding. Earth Surface Processes and Landforms. 2014;39(9):12731278.CrossRefGoogle Scholar
Eberhardt, E, Stead, D, Coggan, JS. Numerical analysis of initiation and progressive failure in natural rock slopes: the 1991 Randa rockslide. International Journal of Rock Mechanics and Mining Sciences. 2004;41:6987.CrossRefGoogle Scholar
Hewitt, K, Clague, JJ, Orwin, JF. Legacies of catastrophic rock slope failures in mountain landscapes. Earth-Science Reviews. 2008;87(1–2):138.CrossRefGoogle Scholar
Hampel, A, Hetzel, R, Maniatis, G. Response of faults to climate-driven changes in ice and water volumes on Earth's surface. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences. 2010;368(1919):25012517.CrossRefGoogle ScholarPubMed
Leith, K, Moore, JR, Amann, F, Loew, S. In situ stress control on the development of near-surface extensional fractures in alpine landscapes. Journal of Geophysical Research, Solid Earth. 2014;119:122.Google Scholar
Ustaszewski, M, Hampel, A, Pfiffner, O. Composite faults in the Swiss Alps formed by the interplay of tectonics, gravitation and postglacial rebound: an integrated field and modelling study. Swiss Journal of Geosciences. 2008;101(1):223235.CrossRefGoogle Scholar
McColl, ST, Davies, TRH. Large ice-contact slope movements: glacial buttressing, deformation and erosion. Earth Surface Processes and Landforms. 2013;38(10):11021115.CrossRefGoogle Scholar
Ballantyne, CK Paraglacial geomorphology. Quaternary Science Reviews. 2002;21(18–19):19352017.CrossRefGoogle Scholar
Stewart, IS, Sauber, J, Rose, J. Glacio-seismotectonics: ice sheets, crustal deformation and seismicity. Quaternary Science Reviews. 2000;19(14–15):13671389.CrossRefGoogle Scholar
Eckardt, P, Funk, HP, Labhart, T. Postglaziale Krustenbewegungen an der Rhein-Rhone-Linie. Vermessung, Photogrammetrie, Kulturtechnik. 1983;2: 4356.Google Scholar
Hippolyte, J-C, Brocard, G, Tardy, M, et al. The recent fault scarps of the Western Alps (France): tectonic surface ruptures or gravitational sackung scarps? A combined mapping, geomorphic, levelling, and 10Be dating approach. Tectonophysics. 2006;418(3–4):255276.CrossRefGoogle Scholar
Hippolyte, J-C, Bourlès, D, Braucher, R, et al. Cosmogenic 10Be dating of a sackung and its faulted rock glaciers, in the Alps of Savoy (France). Geomorphology. 2009;108(3–4):312320.CrossRefGoogle Scholar
von Poschinger, A, Wassmer, P, Maisch, M. The Flims rockslide: history of interpretation and new insights. Landslides from massive rock slope failure. NATO Science Series. 2006;49:329356.CrossRefGoogle Scholar
Meigs, A, Krugh, WC, Davis, K, Bank, G. Ultra-rapid landscape response and sediment yield following glacier retreat, Icy Bay, southern Alaska. Geomorphology. 2006;78(3–4):207221.CrossRefGoogle Scholar
Augustinus, P. Rock mass strength and the stability of some glacial valley slopes. Zeitschrift Fur Geomorphologie. 1995;39(1):5568.CrossRefGoogle Scholar
Cossart, E, Braucher, R, Fort, M, Bourles, DL, Carcaillet, J. Slope instability in relation to glacial debuttressing in alpine areas (Upper Durance catchment, southeastern France): evidence from field data and 10Be cosmic ray exposure ages. Geomorphology. 2007;95(1–2):326.CrossRefGoogle Scholar
Selby, MJ. Controls on the stability and inclinations of hillslopes formed on hard rock. Earth Surface Processes and Landforms. 1982;7(5):449467.CrossRefGoogle Scholar
Bahat, D, Grossenbacher, K, Karasaki, K. Mechanism of exfoliation joint formation in granitic rocks, Yosemite National Park. Journal of Structural Geology. 1999;21(1):8596.CrossRefGoogle Scholar
Ballantyne, C, Sandeman, GF, Stone, JO, Wilson, P. Rock-slope failure following Late Pleistocene deglaciation on tectonically stable mountainous terrain. Quaternary Science Reviews. 2014;86(15):144157.CrossRefGoogle Scholar
Prager, C, Zangerl, C, Patzelt, G, Brandner, R. Age distribution of fossil landslides in the Tyrol (Austria) and its surrounding areas. Natural Hazards and Earth Systems Science. 2008;8(2):377407.CrossRefGoogle Scholar
Cruden, DM, Hu, XQ. Exhaustion and steady state models for predicting landslide hazards in the Canadian Rocky Mountains. Geomorphology. 1993;8(4):279285.CrossRefGoogle Scholar
Strasser, M, Monecke, K, Schnellmann, M, Anselmetti, FS. Lake sediments as natural seismographs: a compiled record of Late Quaternary earthquakes in Central Switzerland and its implication for Alpine deformation. Sedimentology. 2013;60(1):319341.CrossRefGoogle Scholar
McColl, ST. Paraglacial rock-slope stability. Geomorphology. 2012;153–154:116.CrossRefGoogle Scholar
Soldati, M, Corsini, A, Pasuto, A. Landslides and climate change in the Italian Dolomites since the Late glacial. Catena. 2004;55(2):141161.CrossRefGoogle Scholar
Nicolussi, K, Kaufmann, M, Patzelt, G, J van der, Thurner, A. Holocene tree-line variability in the Kauner Valley, Central Eastern Alps, indicated by dendrochronological analysis of living trees and subfossil logs. Vegetation History and Archaeobotany. 2005;14(3):221234.CrossRefGoogle Scholar
Jerz, H, Poschinger, Av. Neuere Ergebnisse zum Bergsturz Eibsee-Grainau. Geologica Bavarica. 1995;99:383398.Google Scholar
Tinner, W, Kaltenrieder, P, Soom, M, et al. The postglacial rockfall in the Kander valley (Switzerland): age and effects on palaeo-environments. Ecologae Geologicae Helvetiae. 2005;98(1):8395.CrossRefGoogle Scholar
Fischer, L, Amann, F, Moore, JR, Huggel, C. Assessment of periglacial slope stability for the 1988 Tschierva rock avalanche (Piz Morteratsch, Switzerland). Engineering Geology. 2010;116(1–2):3243.CrossRefGoogle Scholar
Gruber, S, Haeberli, W. Permafrost in steep bedrock slopes and its temperature-related destabilization following climate change. Journal of Geophysical Research – Earth Surface. 2007;112(F2):F02S13.CrossRefGoogle Scholar
Allen, SK, Gruber, S, Owens, IF. Exploring steep bedrock permafrost and its relationship with recent slope failures in the Southern Alps of New Zealand. Permafrost and Periglacial Processes. 2009;20:345356.CrossRefGoogle Scholar
Ravanel, L, Deline, P. La face ouest des Drus (massif du Mont-Blanc). Évolution de l'instabilité d'une paroi rocheuse dans la haute montagne alpine depuis la fin du petit age glaciaire. Geomorphologie. 2008;4:261272.CrossRefGoogle Scholar
Pogrebiskiy, MI, Chernyshev, SN. Determination of the permeability of the frozen fissured rock massif in the vicinity of the Kolyma Hydroelectric Power Station. Cold Regions Research and Engineering Laboratory. 1977;634:113.Google Scholar
Tang, GZ, Wang, XH. Modeling the thaw boundary in broken rock zones in permafrost in the presence of surface water flows. Tunnelling and Underground Space Technology. 2006;21(6):684689.CrossRefGoogle Scholar
Murton, JB, Peterson, R, Ozouf, J-C. Bedrock fracture by ice segregation in cold regions. Science. 2006;314:11271129.CrossRefGoogle ScholarPubMed
Hallet, B, Walder, JS, Stubbs, CW. Weathering by segregation ice growth in microcracks at sustained sub-zero temperatures: verification from an experimental study using acoustic emissions. Permafrost and Periglacial Processes. 1991;2:283300.CrossRefGoogle Scholar
Dahlström, L-O. Rock Mechanical Consequences of Refrigeration. Göteborg: Chalmers University of Technology; 1992.Google Scholar
Li, N, Zhang, P, Chen, Y, Swoboda, G. Fatigue properties of cracked, saturated and frozen sandstone samples under cyclic loading. International Journal of Rock Mechanics & Mining Sciences. 2003;40:145150.CrossRefGoogle Scholar
Dwivedi, RD, Singh, PK, Singh, TN, Singh, DP. Compressive strength and tensile strength of rocks at sub-zero temperature. Indian Journal of Engineerings and Materials Sciences. 1998;5(1):4348.Google Scholar
Glamheden, R. Thermo-Mechanical Behaviour of Refrigerated Caverns in Hard Rock. Göteborg: Chalmers University of Technology; 2001.Google Scholar
Inada, Y, Yokota, K. Some studies of low-temperature rock strength. International Journal of Rock Mechanics and Mining Sciences. 1984;21(3):145153.CrossRefGoogle Scholar
Dwivedi, RD, Soni, AK, Goel, RK, Dube, AK. Fracture toughness of rocks under sub-zero temperature conditions. International Journal of Rock Mechanics & Mining Sciences. 2000;37:12671275.CrossRefGoogle Scholar
Sanderson, T. Ice Mechanics and Risks to Offshore Structures. Amsterdam: Springer; 1988.Google Scholar
Davies, MCR, Hamza, O, Lumsden, BW, Harris, C. Laboratory measurements of the shear strength of ice-filled rock joints. Annals of Glaciology. 2000;31:463467.CrossRefGoogle Scholar
Arenson, L, Springman, S, Sego, DC. The rheology of frozen soils. Applied Rheology. 2007;17:114.CrossRefGoogle Scholar
Arenson, LU, Springman, S. Triaxial constant stress and constant strain rate test on ice-rich permafrost samples. Canadian Geotechnical Journal. 2005;42:412430.CrossRefGoogle Scholar
Ballantyne, CK, Stone, JO. Timing and periodicity of paraglacial rock-slope failures in the Scottish Highlands. Geomorphology. 2013;186:150161.CrossRefGoogle Scholar
Hovius, N, Lague, D, Dadson, S. Processes, rates and patterns of mountain belt erosion. In: Owens, PN, Slaymaker, O (eds) Mountain Geomorphology. London: Arnold; 2004.Google Scholar
Brunsden, D, Thornes, JB. Landscape sensitivity and change. Transactions of the British Institute of Geographers. 1979;4(4):463484.CrossRefGoogle Scholar
Brunsden, D. Relaxation time. In: Goudie, A (ed.) Encyclopedia of Geomorphology. London: Routledge; 2004. pp. 838840.Google Scholar
Kemeny, J. The time-dependent reduction of sliding cohesion due to rock bridges along discontinuities: a fracture mechanics approach. Rock Mechanics and Rock Engineering. 2003;36(1):2738.CrossRefGoogle Scholar
Haeberli, W, Wegmann, M, Vonder Mühll, D. Slope stability problems related to glacier shrinkage and permafrost degradation in the Alps. Eclogae Geologicae Helvetiae. 1997;90(3):407414.Google Scholar
Harris, C, Arenson, LU, Christiansen, HH, et al. Permafrost and climate in Europe: monitoring and modelling thermal, geomorphological and geotechnical responses. Earth-Science Reviews. 2009;92(3–4):117171.CrossRefGoogle Scholar

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