
Lesson 7 of 8
Antarctica: The frozen time capsule
The land that belongs to no one


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More on The Seven Continents
Lesson 1 of 8
Africa: The continental giant

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Asia: The monsoon continent

Lesson 3 of 8
Europe: The land of contrasts

Lesson 4 of 8
North America: The climate giant

Lesson 5 of 8
South America: Where extremes meet

Lesson 6 of 8
Australia: Life on the edge

Lesson 7 of 8
Antarctica: The frozen time capsule

Lesson 8 of 8 • Quiz
Continents face-off

Common questions
Why is Antarctica so cold?
Antarctica is so cold mainly because it sits at a very high elevation and is surrounded by open ocean rather than warmer land, which keeps warm air masses away. Its thick ice sheet also reflects most incoming sunlight back into space, keeping the surface cold even during the sunlit summer months.
Do people live in Antarctica?
Yes, but not permanently. Antarctica has never had a native population, and no one holds citizenship there. Instead, several thousand scientists and support staff move through its research stations each year, with numbers dropping sharply once winter darkness sets in and travel becomes impossible.
Who owns Antarctica?
No single country owns Antarctica. Several nations made territorial claims in the early twentieth century, but a 1959 international treaty set those claims aside and opened the continent to peaceful scientific research instead, so no government exercises full sovereignty over any part of it today.
Why is Antarctica a desert?
Antarctica counts as a desert because its interior receives extremely little snowfall each year, far less than most sandy deserts get in rain. The freezing air simply cannot hold much moisture, so even though ice covers nearly the entire continent, almost none of it arrives as fresh precipitation.
How much freshwater is stored in Antarctic ice?
Roughly seventy percent of the world's fresh water is frozen inside Antarctica's ice sheet. That ice also makes up about ninety percent of all the ice on Earth, built up gradually over hundreds of thousands of years as snow compressed into solid layers beneath its own weight.