地理漫步·世界地理英语30篇(3)
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The Himalayas: Where Tectonics Meet Tradition
喜马拉雅山脉:构造运动与传统的交汇之地
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The Himalayas formed 50 million years ago when the Indian Plate collided with Eurasia—and they’re still rising about 5 mm per year.
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Mount Everest grows taller each year, yet erosion from glaciers and monsoon rains constantly reshapes its slopes.
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Sherpa communities in Nepal have developed altitude-adapted genetics and traditional weather lore passed down orally for centuries.
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Glaciers here feed ten major Asian rivers, including the Ganges, Indus, and Brahmaputra, sustaining over 1.5 billion people.
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Warmer temperatures are causing glacial lakes to expand rapidly, increasing landslide-dam burst risks downstream.
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Buddhist monasteries often sit on stable bedrock above active faults, reflecting generations of observational site selection.
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Hydropower projects in Bhutan export clean electricity to India, balancing economic needs with fragile mountain ecology.
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Scientists combine satellite imagery with local yak-herder reports to track snowline retreat in remote valleys.