Frost action is the common type of weathering in Temperate Regions and high mountains due to the expansion of freezing water on rocks.
Frost action is the type of weathering common in Temperate Regions and high mountains. This process occurs due to the expansion of water when it freezes, exerting pressure on rocks and leading to their breakdown.
In areas with effective frost wedging, such as higher elevations, talus slopes are often formed as rocky fragments are dislodged by frost action.
Hydration and oxidation are other types of weathering processes that are not as common in these regions compared to frost action.
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