Glacial Formations

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Corrie

Arête

  • Snow accumulates on slope
  • Ice grows into rock (nivation)
  • More accumulation
  • Mass increases, causing it to move downhill
  • Takes the rock with it
  • Leaving a hollow
  • Rotational movement of material causes plucking, making it steeper
  • Debris from plucking and weathering helps to abrade the hollow making it deeper
  • Two corries back to back

Pyramidal Peak

U Shaped Valleys

  • 3 or more worries back to back on a mountain
  • As the glacier moves out of the corrie it causes the valley shape to change from a V to a U
  • Plucking and abrasion occur, causing the valley to deepen and widen
  • Can't flow past interlocking spurs, so instead cut through them, forming steed truncated spurs

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