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Permafrost

Adapted from Wikipedia · Explorer experience

Scientists exploring permafrost in Alaska, studying the frozen ground in a subarctic landscape.

What Is Permafrost?

Permafrost is ground that stays very cold for a long time. It stays below 0 °C (32 °F) for at least two years. You can find it in very cold places like Alaska, Canada, Greenland, and Siberia. Some permafrost has been frozen for hundreds of thousands of years!

Where Is Permafrost Found?

Permafrost is mostly found in the Northern Hemisphere. It is under layers of soil that freeze in winter and melt in summer. This top layer is called the active layer. In some places, the permafrost is very deep, more than 1,400 meters! It is found under soil, rock, and even underwater sediment.

How Much Permafrost Is There?

Permafrost covers about 15% of the land in the Northern Hemisphere that isn’t covered in ice. Here are some big places with lots of permafrost:

LocalityArea
Qinghai-Tibet Plateau1,300,000 km² (500,000 mi²)
Khangai-Altai Mountains1,000,000 km² (390,000 mi²)
Brooks Range263,000 km² (102,000 mi²)
Siberian Mountains255,000 km² (98,000 mi²)
Greenland251,000 km² (97,000 mi²)

Why Do We Care About Permafrost?

Permafrost is important for our world. It holds old plants and animals that have been kept safe by the cold. But as the Earth gets warmer, some permafrost is starting to melt. This melting can change the land. It can make the ground unstable, which can affect buildings and roads. Scientists are studying permafrost to learn more about how it affects our planet and its climate change.

Images

A map showing permafrost and ground ice conditions around the Arctic region.
A scientific diagram showing how subsea permafrost has changed from the Last Glacial Maximum to today.
A scientific diagram showing how massive ground ice is stored in permafrost soil layers.
A large deposit of blue ice found in the permafrost on Herschel Island, Yukon, Canada.
A large cliff on Herschel Island showing layers of ice within the ground, highlighting the effects of thawing permafrost.
A natural ice formation in a pingo in the Mackenzie River delta.
Stone rings formed by permafrost in the Arctic region of Svalbard, Norway.
Natural patterned ground formations shaped like polygons in Padjelanta National Park, Sweden.
A natural ice wedge formation in the Arctic region of Svalbard.
A natural landscape showing permafrost and soil movement in Svalbard's Arctic region.
A scientific diagram showing how temperatures change with depth in permafrost areas, helping us understand Earth's cold regions.
An aerial view of natural ice mounds called palsas, formed by ice lenses in the ground.
Aerial view of pingos, which are large, mound-like formations found in the Arctic, near Tuktoyaktuk, Canada.
A natural pattern formed by frost in Arctic soil, known as permafrost polygons.

Related articles

This article is a child-friendly adaptation of the Wikipedia article on Permafrost, available under CC BY-SA 4.0.

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