Kısaca
The Himalayas aren’t ‘finished’ mountains—they’re a living record of a continental collision. As plates keep pushing, some peaks can rise by centimeters over time.
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Kısaca
The Himalayas aren’t ‘finished’ mountains—they’re a living record of a continental collision. As plates keep pushing, some peaks can rise by centimeters over time.
While a mountain’s windward side gets soaked, the other side can dry out. Air rises, drops rain, then descends, warms, and loses moisture—creating a rain shadow.
Contrary to popular belief, the Great Wall is too thin to be seen from space with the naked eye.
The rocks at the bottom of the Grand Canyon are about half as old as Earth.
Sun warms the surface by day; at night the surface loses heat by radiating it into space. Clouds, humidity, and wind change this ‘heat escape,’ making some nights biting and others mild.
A riverbed isn’t as fixed as it looks. When rains swell flow, sand and gravel move; bends shift, and a river can abandon an old path and carve a new one.
We picture sand, but deserts are defined by rainfall. Antarctica gets so little precipitation it’s technically a vast desert—its snow cover simply hides the fact.
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