Glaciers Ch. 17 Flashcards
Glacier
thick mass of ice
formation
snow flakes, granular snow, firn, glacial ice
Occurs within the ice
• Under pressure, ice is plastic
Internal deformation
• Entire ice mass slipping
along the ground
BASAL SLIP
Acts like a hydraulic jack,
lifting ice to move over rock
MELT WATER
Zone of fracture
- Upper 50 metres
* Tension causes crevasses to form in brittle ice
surges
RAPID MOVEMENT
ice advances
if accumulation exceeds loss
Zone of accumulation
where the glacier forms
zone of ablation
where there is a net loss to the glacier
• Lower limit is the equilibrium line
Calving –
breaking off of large pieces of ice into water
abration
Rocks in ice acting like sandpaper
• Produces rock flour and glacial striations
plucking (hint base of glacier)
Lifting and transport of rock blocks (Erratics) at the base of the glacier
hanging valleys
ABOVE GLACIER
lacial trough (U shaped)
• Transformed by deepening,
widening & straightening