Ice has a simple crystal structure and a fascinating array of physical features that are comparable to features in natural rocks. In this presentation, the underlying principles of ice deformation and its physical behaviour are developed as they apply to the movement of glaciers. Best viewed using Internet Explorer 5 with QuickTime and Flash plug-ins.

Created: August 23, 1999 Authorised by: Head, School of Earth Sciences. Property of The School of Earth Sciences, The University of Melbourne, Australia. Disclaimer and copyright. Created and maintained by Hadi Sim (hadims@unimelb.edu.au).