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Ablation refers to the loss of ice or snow from a glacier. This occurs through processes like melting, evaporation, and calving (when icebergs break off). In warmer regions, melting is the primary cause of ablation, while in colder, polar areas, calving is more significant.12

Glaciation is the process by which glaciers form and grow. Glaciers are nourished by snowfall, and their size depends on the balance between accumulation (gain of mass) and ablation (loss of mass). Glacial erosion, driven by processes like abrasion and plucking, shapes the landscape by carving out features such as striations and U-shaped valleys. Glaciers are classified as temperate or polar based on their temperature regime, which affects their movement and erosive capabilities.134

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