Rupture of an ice mound near Cape Dorset, N.W.T.

An ice feature comprising ice blocks ranging from football size to 0.6 m cubes to 1.2 m × 3.6 m × 0.6 m slabs was observed on the surface of a frozen lake. Site investigations revealed the source of the blocks to be an ice mound that had formed along the shore of the lake. A model, supported by loca...

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Bibliographic Details
Published in:Canadian Geotechnical Journal
Main Author: Frederking, R. M. W.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1979
Subjects:
Online Access:http://dx.doi.org/10.1139/t79-064
http://www.nrcresearchpress.com/doi/pdf/10.1139/t79-064
Description
Summary:An ice feature comprising ice blocks ranging from football size to 0.6 m cubes to 1.2 m × 3.6 m × 0.6 m slabs was observed on the surface of a frozen lake. Site investigations revealed the source of the blocks to be an ice mound that had formed along the shore of the lake. A model, supported by local meteorological, geological, and hydrological information, is proposed to explain the formation of the ice mound and its subsequent rupture.