Physical Uk - Rivers Flashcards
(30 cards)
Features and processes in the upper course
- vertical erosion
- waterfalls
- narrowest part of the river
- slowest flow
Features and processes in the middle course
- lateral erosion
- meanders
- ox bow lakes
- river beach
- deeper water
Features and processes in the lower course
- lateral erosion
- deltas
- floodplains
- deepest water
- fastest flow
Explain how two channel characteristics change along a river’s long profile
1) as river flows from downstream discharge increases due to more water added by tributaries
2) as river flows downstream particle size decreases because as they are transported from upper to lower course more erosion occurs reducing particle size
4 transportation processes
- traction
- saltation
- suspension
- solution
Traction?
Large stones dragged along
Saltation
Small pebbles picked up and dropped
Suspension
tiny particles of sediment carried in the rivers current
Solution (transportation)
Dissolved chemicals carried in solution
4 erosional processes
- abrasion
- attrition
- hydraulic action
- solution
Abrasion
Sand and pebbles dragged along river bed
Attrition
Rocks and stones knock together
Hydraulic action
Fast flowing water forced into cracks breaking up banks
Solution (erosion)
alkaline rocks dissolved by acid rain
Thaweg?
Fastest flow of the river
Helicoidal flow
a flow of water moving material from the outside of one meander bend and depositing it in the inside of the next bend
Levee?
Raised area of land on the banks of the river
3 types of delta
- Niger delta - fan shaped
- Mississippi delta - birdsfoot
- Ebro delta - cuspate
Transpiration?
Water lost through pores in vegetation
Percolation
Water seeping deeper below the surface
infiltration
Water sinking into the soil/rock from the ground surface
Throughflow
Water flowing through soil layer parallel to the surface
Groundflow
Water flowing through rock layer parallel to surface
What are the 3 factors that cause hydrographs to differ?
1) antecedent rainfall - amount of water already in the ground before
2) geology - sandstone/chalk are permeable and absorb water but clay is permeable so surface run off occurs
3) vegetation - rain taken up by plants then evaporates/transpires so never reaches the ground