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A multi-scale resolution of snow-avalanche activity based on geomorphological investigations at Fnjóskadalur, northern Iceland

Published online by Cambridge University Press:  01 May 2013

Armelle Decaulne
Affiliation:
CNRS Geolab UMR6042, University Blaise Pascal Clermont 2, 4 rue Ledru, F-63057 Clermont-Ferrand, France ([email protected])
Thorsteinn Sæmundsson
Affiliation:
Natural Research Centre of Northwestern Iceland, IS-550 Saudárkrókur, Iceland
Ólafur Eggertsson
Affiliation:
Iceland Forest Service, Research Branch, Mógilsá, IS-116 Reykjavík, Iceland

Abstract

The article describes investigations that highlight snow-avalanche events that have not been reported in historical records. While historical sources are most often the basis for all natural hazard and risk research, alternative methods based on geomorphic investigations are often neglected. Here, we emphasise the use of geomorphic evidence to improve our knowledge of the maximum runout distance reached by snow avalanches as well as the frequency of the events. Investigations were carried out in remote, avalanche-prone areas, where the geomorphic evidence has not been disturbed or removed. Dendrogeomorphic investigations supply annual resolved records of avalanche winters up to the age of the investigated tree stand: over 120 years in northern Iceland. The study of snow-avalanche transported debris may be used to map the extent of the potential snow-avalanche deposition zone, and offer relative dating on a secular scale; stratigraphic profiles do provide results on long timescales, but only provide relative dating. The article discusses the relevance of each method, and concludes that the combination of the three methods can improve the common risk-mitigation approach based on historical records.

Type
Research Article
Copyright
Copyright © Cambridge University Press 2013 

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References

Alestalo, J. 1971. Dendrochronological interpretation of geomorphic processes. Fennia 105: 1139.Google Scholar
Bertran, P., and Jomelli, V.. 2004. Avalanches et coulées de slush. In: Bertran, P. (editor). Dépôts de pente continentaux, dynamique et faciès. Quaternaire HS 1: 62–79.Google Scholar
Blikra, L.H., and Nemec, W.. 1998. Postglacial colluvium in western Norway: depositional processes, facies and palaeoclimatic record. Sedimentology 45: 909959.CrossRefGoogle Scholar
Brynjólfsson, S., and Ólafsson, H.. 2009. Precipitation in the Svarfadardalur region, north-Iceland. Meteorology and Atmospheric Physics 103: 5766.CrossRefGoogle Scholar
Corona, C., Lopez Saez, J., Stoffel, M., Bonnefoy, M., Richard, D., Astrade, L. and Berger, F.. 2012. How much of the real avalanche activity can be captured with tree rings? An evaluation of classic dendrogeomorphic approaches and comparison with historical archives. Cold Region Science and Technology 74–75: 3142.CrossRefGoogle Scholar
Corona, C., Rovéra, G., Lopez Saez, J., Stoffel, M. and Perfettini, P.. 2010. Spatio-temporal reconstruction of snow avalanche activity using tree rings: Pierres Jean Jeanne avalanche talus, Massif de l'Oisans, France. Catena 83: 107118.Google Scholar
Decaulne, A. 2005. Slope processes and related risk appearance within the Icelandic Westfjords during the twentieth century. Natural Hazards and Earth Science Systems 3–4: 309318.CrossRefGoogle Scholar
Decaulne, A., Eggertsson, Ó. and Sæmundsson, Th.. 2012. A first dendrogeomorphologic approach of snow avalanche magnitude-frequency in northern Iceland. Geomorphology. doi:10.1016/j.geomorph.2011.11.017.CrossRefGoogle Scholar
Decaulne, A., and Sæmundsson, Th.. 2003. Debris-flow characteristics in the Gleidarhjalli area, north-western Iceland. In: Rickenman, D., and Chen, C.I. (editors). Debris-flow hazards mitigation: mechanics, prediction, and assessment. Rotterdam: Millpress: 11071118.Google Scholar
Decaulne, A., and Sæmundsson, Th.. 2006a. ‘On-zone’ and ‘off-zone’ geomorphic features for multirisk assessment related to slope dynamics in the Icelandic fjords. In: Brebbia, C.A. (editor). Risk Analysis 5. Southampton: WIT Press: 2332.Google Scholar
Decaulne, A., and Sæmundsson, Th.. 2006b. Geomorphic evidence for contemporaneous snow-avalanche and debris-flow impact in the Icelandic Westfjords. Geomorphology 80: 8093.CrossRefGoogle Scholar
Decaulne, A., and Sæmundsson, Th.. 2007. The role of geomorphological evidence for snow-avalanche hazard and mitigation research in northern Icelandic fjords. In: Schaefer, V.R., Schuster, R.L. and Turner, A.K. (editors). First North America landslide conference. AEG publication no. 23: 583592.Google Scholar
Decaulne, A., and Sæmundsson, Th.. 2010. Distribution and frequency of snow-avalanche debris transfer in the distal part of colluvial cones in central north Iceland. Geografiska Annaler 92A (2): 177187.CrossRefGoogle Scholar
Decaulne, A., Sæmundsson, Th. and Jónsson, H.P.. 2008. Extreme runout distance of snow-avalanche transported boulders linked to hazard assessment; some case studies in northwestern and northern Iceland. In: Jónsson, Á., and Jóhannesson, T. (editors). International symposium on mitigative measures against snow avalanches. Egilsstadir, Iceland: The association of Chartered Engineers in Iceland: 131136.Google Scholar
Decaulne, A., Sæmundsson, Th. and Jónsson, H.P.. 2009. An overview of postglacial sediment records from colluvial accumulations in northwestern and north Iceland. Arctic, Antarctic and Alpine Research 41 (1): 3747.CrossRefGoogle Scholar
Decaulne, A., Sæmundsson, Th. and Pétrusson, O.. 2005. Debris flows triggered by rapid snowmelt in the Gleidarhjalli area, northwestern Iceland. Geografiska Annaler 87A (4): 487500.CrossRefGoogle Scholar
Germain, D., Hétu, B. and Filion, L.. 2010. Tree-ring based reconstruction of past snow avalanche events and risk assessment in Northern Gaspé Peninsula (Québec, Canada). In: Stoffel, M., Bollshweiler, M., Butler, D.R. and Luckman, B.H. (editors). Tree-rings and natural hazards: a state-of-the-art. Heidelberg, Berlin, New York: Springer (Advances in Global Change Research 4): 5174.CrossRefGoogle Scholar
Haraldsdóttir, S.H., Tracy, L., Jensen, E.H and Ólafsson, H.. 2006. Avalanches in coastal towns in Iceland. Jökull 56: 125.CrossRefGoogle Scholar
Hewitt, K. 2004. Geomorphic hazards in mountain environments. In: Owens, D., and Slaymaker, O. (editors). Mountain geomorphology. London: Arnold: 187218.Google Scholar
Jakobsson, S.P. 1979. Petrology of recent basalts of the eastern volcanic zone, Iceland. Acta Naturalia Islandica 26: 1103.Google Scholar
Jóhannesson, T., and Jónsson, T.. 1996. Weather in Vestfirdir before and during several avalanche cycles in the period 1949 to 1995. Icelandic Meteorological Office, VÍ-G96015-UR15.Google Scholar
Jomelli, V. 1999. Dépôts d'avalanches dans les Alpes françaises: géométrie, sédimentologie et géodynamique depuis le Petit Age Glaciaire. Géographie Physique et Quaternaire 53: 199209.CrossRefGoogle Scholar
Keylock, C. 1997. Snow avalanches. Progress in Physical Geography 21: 481500.CrossRefGoogle Scholar
Kugelmann, O. 1991. Dating recent glacier advances in the Svarfadardalur-Skídadalur area of northern Iceland by means of a new lichen curve. In: Maizel, J.K., and Caseldine, C. (editors). Environmental changes in Iceland: past and present. Dordrecht: Kluwer Academic Publishers: 203217.CrossRefGoogle Scholar
Luckman, B.H. 1978. Geomorphic work of snow avalanches in the Canadian Rocky Mountains. Arctic and Alpine Research 10: 261276.CrossRefGoogle Scholar
Luckman, B.H. 2010. Dendrogeomorphology and snow avalanche research. In: Stoffel, M., Bollshweiler, M., Butler, D.R. and Luckman, B.H. (editors). Tree-rings and natural hazards: a state-of-the-art. Heidelberg, Berlin, New York: Springer (Advances in Global Change Research 4): 2734.CrossRefGoogle Scholar
McClung, D.M., and Schaerer, P.. 2006. The avalanche handbook. Seattle: The Mountaineers.Google Scholar
McEwen, L.J., Owen, G., Matthews, J.A. and Hiemstra, J.F.. 2011. Late Holocene development of a Norwegian alpine alluvial fan affected by proximal glacier variations, episodic distal undercutting, and colluvial activity. Geomorphology 127: 198215.CrossRefGoogle Scholar
Mears, A. 1980. A fragment flow model of dry avalanches. Journal of Glaciology 26: 153163.CrossRefGoogle Scholar
Schweingruber, F.H. 1996. Tree rings and environment: dendroecology. Bern: Paul Haupt.Google Scholar
Speer, J.H. 2010. Fundamentals of tree-ring research. Tuscon: The University of Arizona Press.Google Scholar
Szymczak, S., Bollschweiler, M., Stoffel, M. and Dikau, R.. 2010. Debris-flow activity and snow avalanches in a steep watershed of the Valais Alps (Switzerland): dendrogeomorphic event reconstruction and identification of triggers. Geomorphology 116: 107114.CrossRefGoogle Scholar
Sæmundsson, Th., Pétursson, H.G. and Decaulne, A.. 2003. Triggering factors for rapid mass movements in Iceland. In: Rickenman, D., and Chen, C.I. (editors). Debris-flow hazards and mitigation: mechanics, prediction, and assessment. Rotterdam: Mill Press: 167178.Google Scholar
Vedurstofa Íslands. 2005. Snjóflódahrina á Vestfjördum 1.–6. janúar 2005 [The snow-avalanche cycle in the Westfjords, 1–6 January 2005]. Reykjavik: Icelandic Meteorological Office (Report 05010).Google Scholar
Ward, R.G.W. 1985. Geomorphological evidence of avalanche activity in Scotland. Geografiska Annaler 67A: 247256.CrossRefGoogle Scholar