Rivers and flooding Flashcards
High elevation terrain
influenced by snowpack and spring hydrology
Alluvial valley
signature of meandering
Stream discharge equation
(Area x velocity x depth )
Drainage trends - moving from headwaters toward outlet
- drainage area and discharge area increase
- slope decreases
- channels become deeper, wider, faster
How much of the streams energy goes into erosion?
3%
Rivers erode rock via:
- abrasion
- plucking
- dissolution
Migration of niagara falls
- destabilization of bedrock at base of falls
- upstream propagation of water (knickpoint)
Dissolved load
river carries mass in solution (ions)
Bedload
particles in contact with riverbed
- rolling
- sliding
Suspended load
particles suspended in flow
Saltation
decreased pressure above particle casues lift
braided streams
- high sediment supply
- multiple channels
- lack of bank stabilization
meandering river
migration via : erosion on outer banks
-deposition on innerbanks
oxbox lakes
Hydrologic response generalities
- lag time
- rising limb
- peak discharge
- recessional limb
How will the hydrograph change for an urbanized watershed?
The lag time will decrease and the peak discharge will increase