Freeze Thaw / Frost Shattering
Temperatures fluctuate around freezing point, water in cracks freezes + expands repeatedly until rock shatters
Frost Heave
Upward movement of soil due to pressure of ice forming underground
Solifluction
Mass movement of active layer downslope
Meltwater Action
Take place in summer when glaciers are melting
Wind Action
Strong wind transports and deposits fine sediment due to lack of vegetation making it easy to pick up