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.
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.
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.
In some coasts there’s water but almost no usable oxygen, forcing life to flee. Excess nutrients trigger algal blooms, then decay consumes oxygen and the area goes quiet.
400 bridges and 150 canals connect these islands. Foundation: wooden poles driven 1000 years ago.
Even if your sky looks calm, there’s a storm somewhere. Earth produces countless electrical discharges at once—we just mistake our horizon for the whole world.
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.
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