Hostname: page-component-cd9895bd7-gxg78 Total loading time: 0 Render date: 2024-12-24T01:40:21.612Z Has data issue: false hasContentIssue false

Glacier ice-cored rock glaciers in the Yukon Territory, Canada?

Published online by Cambridge University Press:  20 January 2017

Wilfried Haeberli*
Affiliation:
Versuchsanstalt für Wasserbau, Hydrologie und Glaziologie, ETH-Zentrum, CH-8092 Zürich, Switzerland
Rights & Permissions [Opens in a new window]

Abstract

Type
Correspondence
Copyright
Copyright © International Glaciological Society 1989

SIR,

An increasing number of measurements, soundings, and drillings has lead to the widely recognized concept that rock glaciers are morphological expressions of creeping mountain permafrost (for example, Reference GorbunovGorbunov, 1983; Reference HaeberliHaeberli, 1985; Reference Barsch and ClarkBarsch, 1988; Reference Belloni, Pelfini and SmiragliaBelloni and others, 1988; Reference Blumstengel and HarrisBlumstengel and Harris, 1988; Reference Carton, Dramis and SmiragliaCarton and others, 1988; Reference Giardino and VitekGiardino and Vitek, 1988; Reference Haeberli and SchmidHaeberli and Schmid, 1988; Reference Haeberli, Huder, Keusen, Pika and RöthlisbergerHaeberli and others, 1988; Reference Cui and ChengZhijiu Cui and Zhu Cheng, 1988; Evin, unpublished). The idea of rock glaciers developing from glaciers has never been based on any firm evidence from appropriate field measurements or reliable model calculations. After reviewing the presently available information from geothermal, electrical resistivity, radio-echo, and seismic refraction soundings, it has been concluded that relations between glaciers and rock glaciers are indirect, accidental, or non-existent (Reference HaeberliHaeberli, 1985, p. 122), and that the idea of an exclusively glacial origin of rock glaciers remains purely speculative (Reference King, Fisch, Haeberli and WaechterKing and others, 1987, p. 94).

In their description of rock glaciers within the Dalton Range, Yukon Territory, Reference Johnson and LacasseJohnson and Lacasse (1988) claimed that rock glaciers form from glaciers which have become totally covered in debris. They made a strong point with this idea, implying that Reference Barsch and ClarkBarsch (1988), Reference GorbunovGorbunov (1983), and myself (Reference HaeberliHaeberli, 1985) have overlooked an obvious and easily recognizable aspect of rock-glacier formation. They wrote that “continuity of glacier ice is visible … from current glaciers through lateral moraines into rock glaciers”. Such reasoning is not new (cf. Reference WhalleyWhalley, 1974, 1979; and earlier papers by P.G. Johnson as quoted by Reference Johnson and LacasseJohnson and Lacasse, 1988), but has repeatedly been criticized (for instance, Reference HaeberliHaeberli, 1985; Reference Barsch, Giardino, Shroder and VitekBarsch, 1987) and does not gain credibility with time. The well-known fact that remains of buried snowbank and glacier ice, as well as other forms of massive underground ice (segregation ice, injection ice; cf. Reference ShumskiyShumskiy, 1955; Reference WashburnWashburn 1979), can be embedded within rock glaciers is not in contradiction to the commonly accepted permafrost model of rock-glacier formation; at the same time, however, the potential inclusion of dead glacier ice by no means implies that rock glaciers as a whole can have a glacial (in contrast to peri-glacial) origin. The observations reported from Dalton Range even fit the concept of periglacial rock glaciers perfectly; the described rock glaciers are in a permafrost condition (Reference Johnson and LacasseJohnson and Laçasse, 1988, p. 331); the reported resistivity of the sub-surface material (10 000–15 000 Ω m; p. 329) is lower than the resistivity values measured in mountain glaciers, snowbanks, or dead glacier ice by several orders of magnitude and is typical for perennially frozen ground rich in ice (cf. Reference HaeberliHaeberli, 1985; Reference King, Fisch, Haeberli and WaechterKing and others, 1987; Evin, unpublished; and the references given in these publications). Finally, the photographs illustrating the article (Reference Johnson and LacasseJohnson and Lacasse, 1988, p. 328, 329) do not show glaciers but a number of snow patches (a common feature of mountain permafrost), the dimensions of which are by orders of magnitude smaller than the dimensions of the discussed rock glaciers.

Johnson and Laçasse must have been aware of these points, because they quoted the corresponding literature. What is then the reason for yet again making a strong statement on the “glacial origin” of rock glaciers, a concept which can obviously not be “understood” but must be “believed” [Inline 1] In view of the numerous definitive studies that have seriously challenged this long-standing belief, and in the absence of solid supportive evidence, Johnson and Lacasse’s claim for a clear glacial origin for the rock glaciers they described has no merit. Moreover, the introduction of their cumbersome term “glacier ice-cored debris-system rock glacier” is unnecessary and most probably misleading.

References

Barsch, D. 1987. The problem of the ice-cored rock glacier. In Giardino, J.R., Shroder, J.F., Vitek, J.D. eds. Rock glaciers. Boston, MA, Alien and Unwin, 4553.Google Scholar
Barsch, D. 1988. Rockglaciers. In Clark, M.J. ed. Advances in periglacial geomorphology. Chichester, etc., John Wiley and Sons, 6990.Google Scholar
Belloni, S. Pelfini, M. Smiraglia, C. 1988. Morphological features of the active rock glaciers in the Italian Alps and climatic correlations. V International Conference on Permafrost in Trondheim. Norway. August 1988. Proceedings, Vol . 1, 678682b.Google Scholar
Blumstengel, W. Harris, S.A. 1988. Observations on an active lobate rock glacier, Slims River Valley, St. Elias Range, Canada. V International Conference on Permafrost in Trondheim , Norway. August 1988. Proceedings, Vol. 1, 689694.Google Scholar
Carton, A. Dramis, F. Smiraglia, C. 1988. A first approach to the systematic study of the rock glaciers in the Italian Alps. V International Conference on Permafrost in Trondheim, Norway, August 1988. Proceedings, Vol. 1, 712717.Google Scholar
Cui, Z. Cheng, Zhu 1988. Rock glaciers in the source region of Urumqi River, middle Tian Shan, China. V Int ernational Conference on Permafrost in Trondheim , Norway. August 1988. Proceedings, Vol, 1, 724727.Google Scholar
Evin, M. Unpublished, Dynamique, repartition et age des glaciers rocheux des Alpes du Sud. (Ph ,D. thesis, Universite de Grenoble I. Institut de Geographie Alpine, 1987.)Google Scholar
Giardino, J.R. Vitek, J.D. 1988. Rock glacier rheology: a preliminary assessment. V International Conference on Permafrost in Trondheim, Norway, August 1988. Proceedings, Vol . 1, 744748.Google Scholar
Gorbunov, A.P. 1983. Rock glaciers of the mountains of middle Asia. Permafrost. Fourth International Conference, July 17-22, 1983. Proceedings. Washington, DC, National Academy Press, 359362.Google Scholar
Haeberli, W. 1985. Creep of mountain permafrost: internal structure and flow of Alpine rock glaciers. Eidg. Tech. Hochschule , Zürich. Versuchsanst . Wasserbau, Hydrol. Glaziol. Mitt. 77Google Scholar
Haeberli, W. Schmid, W. 1988. Aerophotogrammetrical monitoring of rock glaciers. V International Conference Oil Permafrost in Trolldheim , Norway, August 1988, Proceedings, Vol . 1, 764769.Google Scholar
Haeberli, W. Huder, J. Keusen, H.–R. Pika, J. Röthlisberger, H. 1988. Core drilling through rock glacier permafrost. V Internatiollal Conference on Permafrost in Trondheim , Norway , August 1988. Proceedings, Vol . 2, 937942.Google Scholar
Johnson, P.G. Lacasse, D. 1988. Rock glaciers of the Dalton Range, Kluane Ranges, south-west Yukon Territory, Canada. J. Glaciol., 34(118), 327332.CrossRefGoogle Scholar
King, L. Fisch, W. Haeberli, W. Waechter, H.P. 1987. Comparison of resistivity and radio-echo soundings on rock glacier permafrost. Z. Gletscherkd. Glazialgeol., 23(1), 7797.Google Scholar
Shumskiy, P.A. 1955. Osnovy strukturnogo ledovedeniya. Moscow, Izdatel'stvo Akademii Nauk SSSR. [English translation: Principles of structural glaciology. New York, Dover, 1964.]Google Scholar
Washburn, A.L. 1979. Geocryology; a survey of periglacial processes and environments. London, Edward Arnold.Google Scholar
Whalley, W.B. 1974. Rock glaciers and their formation as part of a glacier-debris transport system. Reading, University of Reading. (Geographical Papers 24.)Google Scholar
Whalley, W.B. 1979. The relationship of glacier ice and rock glacier at Grubengletscher, Kanton Wallis, Switzerland. Geogr, Ann., 61A(1-2), 4961.CrossRefGoogle Scholar