Some glaciers have rivers that flow along their flanks or across the terminal face, and are also prone to cliff collapse. Here, the terminal cliff of Childs Glacier, is being undercut by the fast-flowing Copper River in SE Alaska MH.
« Previous · Back to the thumbnails · Next »
Updated 2006-10-09 · © Glaciers online · J. Alean · M. Hambrey
Hosted by Metanet