Frost Wedging

Frost wedging is a geological process where water seeps into cracks in rocks. When temperatures drop, this water freezes and expands, exerting pressure on the surrounding rock. Over time, repeated cycles of freezing and thawing can cause the rock to crack and break apart. This process is particularly effective in areas with frequent temperature fluctuations, and it contributes to the weathering of rocks and the formation of soil. Frost wedging plays a significant role in shaping landscapes, especially in colder climates.