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Glaciation - Coggle Diagram

- - - - Freeze-thaw weathering makes mountain sides jagged. Glacier moves downhill due to gravity.
        
        Bergschrund crevasses (allows meltwater/rock to get to base of glacier adding to erosive power) opens up.
        
        Plucking happens> steepening sides.
        
        Weight of causes rotational sliding > deepening hollow
- - - - Snow compresses into neve>ice.