•the hydrological processes (erosion, transportation deposition) operate within rivers and drainage basins
•erosion:
•hydraulic action: force of wave hits the rock; the air is trapped by a wave in a crack and cracks it further due to hydraulic pressure
•abrasion: where rocks are picked by waves and thrown against the cliff
•solution: where the rock is put into solution by weak acids
•attrition: materials in the wave smash each other, becoming smaller and rounder
•transportation:
•traction: where larger, heavier material that makes up the river’s bedlam is rolled along
•saltation: where the lighter material that makes up the river bedlam is bounced along the river bed
•suspension: where lighter material that makes up the river’s suspended load is carried by the river
•solution: where dissolved material that makes up the river’s solute load in solution
•deposition:
•when river lose energy, it starts to drop it’s bed-load anywhere
•the heaviest material will be deposited first etc.
•deposition occurs: •a decrease in gradient and smoothness
•a decrease in river flow as water drains away after lots of precipitation
•the river meets a large body of water
•the river flowing more slowly on inside bends
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