Wall of Ice, College Glaciers, Alaska

Glaciers are born from snow fields. If the top of a mountain gets, say, 400 feet of snow in the winter, but only 200 feet of it melt in the summer, the snow gets deeper and deeper. In time, the weight of all that snow compresses the bottom layers of snow into ice, and it squeezes the ice out. This image clearly shows the ice flowing down the mountain to the sea.

Print # 9209s99003
Image type: 35mm, 3538x2859

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