terrainfrozen
Terrainfrozen refers to a state where the ground or a large area of land has become solidified and immobile due to freezing temperatures. This phenomenon is most commonly observed in polar regions, high-altitude mountain ranges, and during severe winter conditions in temperate climates. When the water present in soil, rock, or other geological materials freezes, it expands and binds the components together, creating a rigid surface.
The depth and extent of terrainfrozen depend on several factors, including ambient temperature, duration of freezing