Glacial Landscapes in the UK Flashcards
Last Ice Age
18,000 years ago
Erosion: Abrasion
As glacier moves downhill, rocks frozen into base and sides, scrape the rock beneath, leaving scratches called striations behind
Erosion: Plucking
Rocks become frozen into bottom and sides of glacier. As glacier moves downhill, it ‘plucks’ rocks frozen into glacier from ground
Freeze-thaw weathering
Temp. higher at day, so snow melts and water enters cracks in rock. Temp. drops at night, so water freezes, expands, and forces rock to break eventually
Erosion Landforms: Corrie (cirques/cwms)
- Snow collects in sheltered hollow on side of mountain;
- Air squeezed out from compact snow —> ice
- Back wall of corrie gets steeper (freeze-thaw weathering and plucking);
- Base of corrie gets deeper (abrasion);
- Glacier gets heavier and moves downhill, out of hollow in circular motion (rotational slip);
- Less erosion at from of glacier —> corrie lip;
- After glacier melted, a lake forms —> corrie lake or tarn
Corrie Features
Arêtes — narrow ridge, between two corries erode side by side;
Pyramidal Peal — three + corries erode side by side, pointed peak left
Erosion Landforms: Truncated Spurs
Interlocking spurs eroded by plucking and abrasion as glacier moves through an old river valley
Erosion Landforms: Glacial Trough
U-shaped from when glacier melts through truncated spur
Erosion Landforms: Ribbon Lake
Sometimes glacial trough fills with water
Erosion Landforms: Hanging Valley
Old tributaries left suspended
Transportation: Bulldozing
Rocks and debris, found in front of glacier, are pushed downhill by sheer force of moving ice
Transportation: Rotational Slip
Circular movement of ice in corrie
Moraine
Any material carried or moved by glacier and deposited
Lateral Moraine
Material deposited along both sides — made of weathered material fallen from valley sides above glacier
Medial Moraine
Material deposited in middle of glacier — caused by lateral moraines of two glaciers when they meet