Summary
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.
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Summary
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.
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.
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.
As cities expand, they often build on top of older layers—streets rise and history stacks. Underground, old houses, shops, and roads can remain like frozen time.
The rocks at the bottom of the Grand Canyon are about half as old as Earth.
Contrary to popular belief, the Great Wall is too thin to be seen from space with the naked eye.
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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