SEE: Glaciation 2A.7C: Lowland erosional landforms

?
View mindmap
  • 2A.7C: Erosional LOWLAND landforms
    • Ice sheet scouring
      • Process of erosion that occurs when ice sheets flow over lowland
    • Roche-moutonnees
      • Stoss= upstream         Loss= downstream
      • Stoss side
        • 1. Glacier hits obstacle that is too large to be plucked, so moves over it
          • 2. By hitting the obstacle, pressure and friction increases so ice melts
            • 3. This metlwater allows the glacier to slide over the rock
        • There are striations as smaller rocks abrade the surface
          • This is due to abrasion because of the meltwater
      • Lee side
        • 1. As the glacier reaches the lee side, friction and pressure drops
          • 2. This causes the meltwater to refreeze
            • 3. It then sticks to the outcrop, and plucks smaller pieces of rock
              • 4. This leaves a jagged surface on the lee side
      • EXAMPLE: Myot Hill, Scotland
      • Bare outcrop of rock sculpted by erosion
      • Can be 5-30m tall
    • Knock and lochan
      • Lowland landscape of bare, ice sculpted hills (knocks) and small lakes (lochans)
      • 1. Areas of resistant rock are unable to be eroded, forming the knocks
        • 2. Selective, deeper erosion of faults and weaker areas of rocks form the lochans
          • Different geology plays a key role
      • EXAMPLE: Isle of Lewis, Scotland
    • Crag and tail
      • A landform consisting of a rock hill and tapering edge
      • 1. A resistant object prevents flow of the glacier (the crag)
        • 2. Ice is forced around the obstacle, eroding the rock around it
          • 3. This eroded material is then deposited on the lee side to form the tail
      • EXAMPLE: Castle Rock (crag) and Royal Mile (tail) Edinburgh

Comments

No comments have yet been made

Similar Geography resources:

See all Geography resources »See all Hot and cold environments resources »