 Speckle tracking of ALOS Palsar and Radarsat, two datasets has been used to determine the dynamics of major glacier and ice masses in western Canada over the past decade, resulting in spatially comprehensive velocity maps for many regions. Faster flow is generally observed on large ocean and land terminating outlet glacier, particularly those in high accumulation maritime regions. Baseline maps of glacier velocities determined from speckle tracking of SAR datasets are now available for nearly all the major ice masses of Canada. This article was authored by Wesley Van Wychyn, Luke Copeland, Hester Joskeet, and others.