Summary
The rocks at the bottom of the Grand Canyon are about half as old as Earth.
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Summary
The rocks at the bottom of the Grand Canyon are about half as old as Earth.
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.
400 bridges and 150 canals connect these islands. Foundation: wooden poles driven 1000 years ago.
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.
On a historical timescale, the Sahara was green and wetter “yesterday.” As rainfall patterns shifted, lakes shrank—leaving not just sand, but a massive climate story.
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.
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