How Rivers Drain the Landscape: Processes and Pathways
Rivers sculpt and drain terrain through four primary processes:
- Erosion: Hydraulic action, abrasion, and solution wear down bedrock and banks, deepening/widening channels.
- Deposition: Sediment drops where velocity decreases—forming bars, floodplains, deltas.
- Infiltration: Water percolates into permeable beds (sand/gravel), recharging aquifers.
- Evaporation: Direct loss to atmosphere, significant in arid regions.
The dominant process varies by climate, geology, vegetation, and gradient. Together, they shape watersheds and determine water availability.