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This is the force that moves soil down a slope
Frost Wedging
Angle of repose
Chemical
Gravity
Solum or True Soil
Solifluction
Scarp
Mass Wasting
This is the slow, downslope flow of water saturated material in permafrost areas
Frost Wedging
Angle of repose
Chemical
Gravity
Solum or True Soil
Solifluction
Scarp
Mass Wasting
This is the mechanical breakup of rock by the expansion of freezing water in cracks and crevices
Frost Wedging
Angle of repose
Chemical
Gravity
Solum or True Soil
Solifluction
Scarp
Mass Wasting
This is the exposed, crescent shaped ruptured surface at the head of a slump
Frost Wedging
Angle of repose
Chemical
Gravity
Solum or True Soil
Solifluction
Scarp
Mass Wasting
This type of weathering occurs when the internal structure of a mineral is altered.
Frost Wedging
Angle of repose
Chemical
Gravity
Solum or True Soil
Solifluction
Scarp
Mass Wasting
This includes all soil horizons above the C-horizon
Frost Wedging
Angle of repose
Chemical
Gravity
Solum or True Soil
Solifluction
Scarp
Mass Wasting
The down slope movement of rock, regolith, and soil under the direct influence of gravity
Frost Wedging
Angle of repose
Chemical
Gravity
Solum or True Soil
Solifluction
Scarp
Mass Wasting
This is the steepest angle at which loose material remains stationary without sliding
Frost Wedging
Angle of repose
Chemical
Gravity
Solum or True Soil
Solifluction
Scarp
Mass Wasting
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