Ice wedging primarily affects mountainous regions and areas with significant temperature fluctuations, particularly in climates that experience freeze-thaw cycles. It contributes to the formation of features such as rockslides, talus slopes, and other forms of weathered rock. Additionally, ice wedging can shape landscapes in cold environments, leading to the creation of fissures, cracks, and potholes in the ground. Overall, it plays a crucial role in the physical weathering of exposed rock surfaces.
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