Rivers and flooding Flashcards
(18 cards)
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
Suspended load
What makes river dirty
-sand sediments
Difference between braided and meandering rivers
Braided channels change all the time where as meandering is easier to predict where it will change in the future.
Four H’s of salmon decline
- Harvest
- hydro
- hatcheries
- habitat