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Glaciers
A glacier is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. Glaciers slowly deform and flow under stresses induced by their weight, creating crevasses, seracs, and other distinguishing features. They also abrade rock and debris from their substrate to create landforms such as cirques, moraines, or fjords. Glaciers form only on land and are distinct from the much thinner sea ice and lake ice that forms on the surface of bodies of water.
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You've been here before, Bell. Remember the stories you told me about wandering in the woods when you were a little girl? It scared the crap out of you, but you went out there all alone, knee-high to a bunny rabbit, and picked berries and climbed trees and found bird nests and came home all bug-bitten and mossy. And you loved every minute of it. It made you our beautiful Arctic Bell, impervious to cold and feared by mosquitoes. Aren't you glad you didn't stay by grandma's side, darning socks and
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Rising temperatures are boosting evaporation rates, altering rainfall patterns, and melting the glaciers that feed rivers during the dry season.
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― Plan B 3.0: Mobilizing to Save Civilization
― Plan B 3.0: Mobilizing to Save Civilization
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