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Glacial erosion is the process by which glaciers wear away the Earth's surface. This occurs primarily through two mechanisms: abrasion and plucking. Abrasion happens as rocks and debris embedded in the ice grind against the bedrock, creating scratches and polish. Plucking involves the ice freezing onto bedrock and pulling pieces away.12

Temperate glaciers, which are at the melting point of ice, are more effective at erosion due to basal sliding. Polar glaciers, being colder, erode less effectively. Glacial erosion is responsible for shaping many mountainous landscapes, creating features like U-shaped valleys, cirques, arêtes, and horns. It also plays a role in sculpting larger features such as the Great Lakes.34

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