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This is the most abundant weak acid involved in chemical weathering and soil formation
Solum or True Soil
Soil Texture Triangle
Solifluction
Soil Horizons
Carbonic
Scarp
Angle of repose
Residual
This is used to determine the percentages of sand, silt and clay in a soil
Solum or True Soil
Soil Texture Triangle
Solifluction
Soil Horizons
Carbonic
Scarp
Angle of repose
Residual
This is the slow, downslope flow of water saturated material in permafrost areas
Solum or True Soil
Soil Texture Triangle
Solifluction
Soil Horizons
Carbonic
Scarp
Angle of repose
Residual
This is the steepest angle at which loose material remains stationary without sliding
Solum or True Soil
Soil Texture Triangle
Solifluction
Soil Horizons
Carbonic
Scarp
Angle of repose
Residual
This is the exposed, crescent shaped ruptured surface at the head of a slump
Solum or True Soil
Soil Texture Triangle
Solifluction
Soil Horizons
Carbonic
Scarp
Angle of repose
Residual
Soil profiles are divided into different zones or layers called this
Solum or True Soil
Soil Texture Triangle
Solifluction
Soil Horizons
Carbonic
Scarp
Angle of repose
Residual
This is soil that develops on top of bedrock
Solum or True Soil
Soil Texture Triangle
Solifluction
Soil Horizons
Carbonic
Scarp
Angle of repose
Residual
This includes all soil horizons above the C-horizon
Solum or True Soil
Soil Texture Triangle
Solifluction
Soil Horizons
Carbonic
Scarp
Angle of repose
Residual
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