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Stream and Drainage Network Formation
Headward erosion extends channels upstream.
Drainage patterns depend on rock type and structure: dendritic (uniform material), radial (volcanoes), rectangular (faulted terrain).
Stream Work and Landforms:
Erosion (cutting valleys), transport (sediment load), deposition (deltas, alluvial fans).
Changes Along Stream Length:
From headwaters to mouth:
Decrease in sediment size.
Increase in discharge and sediment load.
Floodplain
Low-lying ground next to river, built by sediment deposition during floods.
How discharge will change along the course of a river in a temperate versus arid regions
Temperate: More consistent flow, seasonal floods.
Arid: Ephemeral streams, flash floods after storms.
How is Discharge Changes measured?
Q = A × v where A = cross-sectional area, v = velocity.
Relationship between stream discharge and urbanization.
Increases impermeable surfaces → higher peak discharge, faster runoff, less groundwater recharge.