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to the site. The biggest problem with this system is that if
there are no glide slab releases there is no opportunity for
the probes to return to the vertical position. Although, in
this study no effort has been made to separate glide from
normal avalanches such differentiation could be attained
by using shorter probes. In future studies correlations with
weather activity will be made, this was made difficult with
this data set as the exact times of the recorded avalanches
was not known in many instances. Further design
improvements are necessary such asimproving robustness
of the electrical connections and probes themselves.
Despite the limitations, the probes can pr ovide the
forecaster with additional information about glide cycles
and creep in the snow.

ACKNOWLEDGEMENTS

The authors wish to thank Robin Black, The National Research
Council of Canada, Brant Benum, Scot Davies, Lake Louise
Ski Area and The Sunshine Ski Area for their support during
this project. Wilson and Statham performed this work while
under contract for Mountain Watch Inc.

REFERENCES
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Akitaya, E. and Shimizu, H. Behaviour of a Snow Cover After
Crack Formation on Mountain Slope ISSW 1988 pp179-186

In der Gand, H.R. and Zupancic, M. Snow Gliding and Ava-
lanches International Symposium on Scientific Aspects of
Snow and Ice Avalanches Publication Number 69, 1966,
pp230-242

Langinger, B. Stability and Fracture of the Snow Pack for Glide
Avalanches, Avalanche Formation, Movement and Effects, Pro-
ceedings of the Davos Symposium, IAHS Press Wallingford,
Oxfordshire. IAHS Pub # 162, 1986, pp229-240

McClung D.M. Avalanche Formation, Movement and Effects,
Proceedings of the Davos Symposium, September 1986 IAHS
publication No. 162, 1987, P475-508

McClung, D.M., Bennetto J.D., Walker, S. and Golley W. Snow
Gliding on Steep Rock Coquihalla, B.C. ISSW 1990 pp93-94
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