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☆☆☆☆☆laterite
The capacity of a stream is the maximum load it can carry. Capacity is directly related to a stream's discharge. The greater the volume of water in a stream is, the greater its capacity is for carrying sediment. So if a stream's discharge decreases, the stream's capacity also decreases.
nonpoint source pollution
The 3 main types of glacial erosion are plucking, abrasion and freeze thaw.
Limiting development on floodplains is effective in controlling floods because this allows floodplains to absorb floodwaters without harm to structures
differential weathering
bed load and suspended load
Partially weathered parent material is found in the C horizon of a soil profile.
Rockfall.
In the eastern half of the united states.
Pedalfer
No
the direction of glacial movement 🥶
mass movement
In a typical stream where the gradient is steep the discharge is small.
moisture is lacking and organic acids are scarce ;D
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