Glaciers are slowly-moving rivers of ice propelled forward by
the stress of their own massive weight.
A mass of land ice that is formed by the cumulative recrystallization
of firn. A glacier flows slowly from an accumulation area to an ablation
area. Some well-known glaciers are: the Zermatt, Stechelberg, Grinelwald,
and Les Diablerets in Switzerland; the Nigards, Gaupne, Fanarak, and Lom
in Norway; the Wright Taylor and Wilson Piedmont glaciers in Antarctica;
Grinnell glacier in Glacier National Park, Montana, U.S., and the Teton
glacier in Teton National Park, Wyoming, U.S. |