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Updated: May 4, 2025
In very hot and long summers, the ice-fields are denuded even in the higher regions, and then a much greater amount of blue-green glacier-ice glances down into the valley, many knobs and depressions are laid bare which one otherwise sees only covered with white, the muddy edge of the ice comes to view with its deposit of rocks, silt, and slime, and far greater volumes of water than usual rush into the valley.
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