Frozen Ground

Frozen ground, often referred to as permafrost, is soil or rock that remains at or below freezing temperatures for an extended period, typically two years or more. This condition is commonly found in polar regions, like Alaska and Siberia. The frozen layer can significantly impact local ecosystems, construction, and climate change. As temperatures rise, permafrost can melt, releasing greenhouse gases like methane, which can further contribute to global warming. Understanding frozen ground is crucial for predicting environmental changes and managing infrastructure in affected areas.