River processes and pressure Flashcards
Hydraulic action
The force of the water on the bed and banks of the river removes material
Attrition
The load that is carried by the river bumps together and wears down into smaller, smoother pieces
Abrasion
Material carried by the river rubs against the bed and banks and wears them away
Solution
Some rock minerals dissolve in river water (e.g. calcium carbonate in limestone)
Traction
Large boulders roll along the river bed
Saltation
Smaller pebbles are bounced along the river bed, picked up and then dropped as the flow of the river changes
Suspension
Finer sand and silt particles are carried along in the flow, giving the river a brown appearance
Solution
Minerals from rocks such as limestone and chalk, are dissolved in the water and carried along in the flow, although they cannot be seen
Deposition
When the river loses energy (slows down) it may drop some of its load
How are waterfalls formed (upper course feature)?
1- Band of more resistant rock lies over less resistant rocks
2- Less resistant rock is eroded more quickly, leaving a ‘step’ - the waterfall
3- More resistant rock is undercut, forming an overhang
4- Overhang can no longer be supported, blocks of rock fall down
5- Powerful fall of water erodes plunge pool using fallen rocks
6- Waterfall retreats upstream
How are interlocking spurs formed (upper course feature)?
- The river at its source is small and has limited energy. - It flows naturally from side to side, around ridges in the valley sides, called spurs
- The spurs become interlocking with those on the other side of the valley
How are meanders formed (lower course feature)?
- they are bends in the river’s course
- in the lower course, the river uses up surplus energy by swinging one way to the other, causing lateral erosion on the outside of bends and deposition on the inside
How are do bow lakes formed (lower course feature)?
- forms when a river creates a meander, due to the river’s eroding bank
- after a long period of time, the meander becomes very curved, and eventually the neck of the meander becomes narrower
- the river cuts through the neck during a flood, cutting off the meander and forming an oxbow lake
Explain how erosion and deposition form floodplains (lower course feature) (4)?
- as a river meanders in its lower course, lateral erosion erodes away the valley sides, making the valley flatter
- the meanders migrate downstream
- at the same time, deposition occurs as every time the river floods, fine particles of silt are deposited onto the valley sides, forming the floodplain over thousands of years
How are levées formed (lower course feature)?
- as the river floods over its bank, the water slows down
- the water can’t carry the biggest + heaviest silt particles and thyme are dropped straight away on the bank forming flood plains
- increased deposition on the river bed when the river is low gradually raises the river bed upwards
- after many floods, the deposits on the bank build up, forming levées