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Glaciation

Year 9 πŸ”οΈ Physical Geography  Glacial processes, landforms, and glacial environments.

❄️ Glacial Processes

Glaciers shape landscapes through erosion, transportation, and deposition.

Freeze-Thaw Weathering

Water enters cracks, freezes and expands, shattering rock (frost shattering). Provides angular material for glaciers.

Abrasion

Rock fragments embedded in glacier act as sandpaper, grinding and smoothing the rock below. Creates smooth, striated surfaces.

Plucking

Meltwater freezes around rock outcrops. As ice moves, rock is torn away. Creates jagged, uneven terrain.

Ice Movement

Rotational sliding (in corries) and basal sliding (lubricated by meltwater). Ice deforms internally under pressure.

πŸ”οΈ Glacial Landforms

Glaciers create distinctive erosional and depositional landforms.

Corrie (Cirque)

Armchair-shaped hollow on mountainside. Formed by rotational sliding and freeze-thaw. Contains a tarn (lake).

U-Shaped Valley

Glacier widens and deepens a V-shaped river valley. Steep sides, flat floor. Hanging valleys at tributary mouths.

ArΓͺte

Knife-edge ridge between two corries or U-valleys, carved from both sides.

Moraine & Drumlins

Moraine = glacial deposits. Terminal moraine at furthest extent. Drumlins = elongated mounds of till, blunt end faces ice.

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πŸ—ΊοΈ Interactive Exploration β€” Glaciation
πŸ“Š Data Analysis β€” Glaciation
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