Cryosphere elements educational scheme with ice and water outline diagram. Snow cap, glacier, permafrost and iceberg location description as geological pole and antarctica parts vector illustration.

When glaciers and ice sheets melt, they can destabilize slopes and reactivate faults, which in turn can trigger landslides and reshape the surface of Earth over long periods of time. Researchers ...

An inevitable, and observable, consequence is the thawing of permafrost, and there are strong indications that the occurrence of landslides is increasing as consequence. However, there is still ...

See our Citation Policies for more details about how to structure your data citation. This data set consists of a geo-referenced digital map and attribute data derived from the publication 'Permafrost ...

Instead, they were delayed by several thousand years, until permafrost began thawing. The researchers say their findings indicate that thawing permafrost was an important trigger of landslides in ...

Infrastructure in permafrost areas is threatened by river bank erosion, Mackenzie River Delta, Canada. Credit: Angus Alunik, 2021 The first comprehensive study examining the social impacts of thawing ...

A while later, scientists became interested and persuaded Shergin to keep digging. After ten years, the mine had reached its present depth of 116 meters, and Yakutsk became known as the cradle of ...

Instead, they were delayed by several thousand years, until permafrost began thawing. The researchers say their findings indicate that thawing permafrost was an important trigger of landslides in ...

Researchers are now attempting to integrate new strategies to monitor permafrost and prevent its further melting. Researchers with the European Space Agency’s Climate Change Initiative (CCI) project ...

Utilizing over three decades of geospatial data, researchers pinpointed areas where permafrost, critical to the global climate, is in jeopardy due to increased warming and drying, highlighting the ...

Le Permafrost, ou pergélisol en français, est un sous-sol gelé en permanence dont la température n’excède pas 0 °C pendant au moins deux années consécutives.