Mount Rainier National Park

Mount Rainier National Park

Land of Ice

Volcanic activity built Mount Rainier, but it is glaciers that shape it. True glaciers consist of at least three layers: snow, mixed snow and ice, and pure ice. They are formed because the mountain's winter snowfall surpasses its summer snowmelt. Season after season, the snowpack accumulates and its weight compresses the snow below into glacier ice. 

Heavy snow accumulation expands the glacier, with its weight pushing and moving the existing ice. This is offset by melting at the terminus (or snout) of the glacier. Glaciers are called "rivers of ice" because they move down the steep mountain valleys, ebbing and flowing with climatic conditions. The rate of movement varies, depending on the rate of snowfall and snowmelt. Mount Rainier's glaciers move from just a few inches up to two feet per day, depending on the steepness of the slope. Great crevasses open in the glacier when stresses on the ice cause it to separate. 

More than 35 square miles of glaciers radiate out from Mount Rainier's summit, the largest collection of glaciers on one peak in the contiguous U.S. The mountain has 26 named glaciers and numerous smaller, unnamed glaciers and ice fields.