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Erosion and Deposition

Erosion and Deposition. Glaciers. Glaciers. Glacier - a large mass of ice that moves over land Alpine glaciers – occur in mountain and are erosional Continental glaciers – occur on flatter land and are mostly depositional. Glaciers.

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Erosion and Deposition

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  1. Erosion and Deposition • Glaciers

  2. Glaciers • Glacier - a large mass of ice that moves over land • Alpine glaciers – occur in mountain and are erosional • Continental glaciers – occur on flatter land and are mostly depositional.

  3. Glaciers • Glaciers occur in a cold region where more snow falls than melts each year. • In alpine glaciers the weight of the heavy mass of ice causes it to flow downward slowly. • A continental glacier spreads out under its own weight.

  4. Alpine Glaciers • Cirque – a bowl-shaped erosion near the top of a mountain caused by a glacier through ice wedging. • Horn – a sharp peak where 3 or 4 cirques come together. • Arete – a ridge that forms where 2 cirques come together. • Alpine glaciers create U-shaped valleys.

  5. Moraines • Till – different sized sediments deposited by a glaciers. • Moraine – a deposit left behind by a retreating glacier. • End moraine – left at the end or toe of a glacier. • Lateral moraine – left at the sides of a glacier. • Medial moraine – left in the middle, where two glaciers come together.

  6. Glaciers • Kettle – occurs when a large chunk of ice becomes buried in the soil. When the glacier retreats, the ice melts forming a lake. • Esker – a sinuous ridge of sorted till that forms as sediment is laid in a river that forms on or under a glacier. • Kame – a mound of sort till that forms in a lake that form on a glacier.

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