β the force of the water π
β³ compresses air trapped in the bank π¨
β creating an explosive blast π₯
(causing materials to be dislodged)
β force of the water π
β³ throws bedload against the banks πͺ¨
β wearing them down
β Acidity of the water π
β³ dissolves the rocks π§ͺπͺ¨
BEGINNING:
1.) β Waterfalls π
β³ are found where:
* soft rock (e.g. clay - less resistant) πͺ¨
is beneath
* hard rock (e.g. granite - more resistant) πͺ¨
MIDDLE (PROCESSES):
2.) β Erosion occurs through:
* ‘hydraulic action’ π
β (the force of water compresses air trapped in the bank, creating an explosive blast, causing materials to be dislodged π₯)
* ‘abrasion’
β (the force of water throws bedload against the banks, wearing them down πͺ¨)
* ‘solution’
β (acidity in the water dissolves the rocks π§ͺ)
ENDING (FINAL PROCESSES):
3.) β Overtime,
* the water is able to erode the underlying soft rock more quickly than the hard rock (as it’s weaker)
β DIFFERENTIAL EROSION,
4.) β As the soft rock is eroded,
* it forms an OVERHANG of hard rock & a PLUNGE POOL
β where the weaker, softer rock is eroded more deeply.
5.) β Overtime, the overhang collapses due to:
* it’s own weight (as it’s unsupported)
* and the effect of gravity
β this causes the waterfall to retreat upstream.
6.) β The resulting debris can increase the erosion of the plunge pool
β by increasing erosive power
BEGINNING:
1.) β The river channel erodes downwards
β due to VERTICAL EROSION
MIDDLE (PROCESSES):
2.) β Erosion occurs through:
1. ‘hydraulic action’
β (the force of water compresses air trapped in the bank, creating an explosive blast, causing materials to be dislodged π₯)
2. ‘abrasion’
β (the force of water throws bedload against the banks, wearing them down πͺ¨)
3. ‘solution’
β (acidity in the water dissolves the rocks π§ͺ)
ENDING (FINAL PROCESSES):
3.) β The river only erodes a small section of the valley
4.) β Material is moved down the valley sides by MASS MOVEMENT
β for example, FROST HEAVE (expansion and contraction of soil, due to changing temperatures, dislodges soil) and gravity.
5.) β This material adds to the erosive power of the river
β increasing erosion of the river bed.
BEGINNING:
1.) In a straight river channel, water turns around obstructions (such as boulders)
β³ resulting in areas of slower (pools) and faster (riffles) water (as it becomes more sinuous)
2). Riffles & pools π
β³ lead to changes in speed & depths in the river channel
β as pools are deeper whereas riffles are shallower
(with greater turbulence)
MIDDLE (PROCESSES):
3.) Erosion occurs through:
1. ‘hydraulic action’
β (the force of water compresses air trapped in the bank, creating an explosive blast, causing materials to be dislodged π₯)
2. ‘abrasion’
β (the force of water throws bedload against the banks, wearing them down)
3. ‘solution’
β (acidity in the water dissolves the rocks π§ͺ)
ENDING (FINAL PROCESSES):
4.) Rivers flow fastest on the outside bend
β³ as there is increasing erosive power β‘
(causing undercutting & the formation of river cliffs)
5.) Rivers flow slowest on the inside bend
β³ leading to deposition β³
6.) HELICOIDAL FLOW πͺ
β³ transfers sediment from the river cliffs to river beaches in a corkscrew movement
7.) Meanders migrate downwards
β³ as erosion continues.
BEGINNING:
1.) Riffles & pools
β³ lead to changes in speed and depth in the river channel
β as pools are deeper, whereas, riffles are shallower (with greater turbulence)
MIDDLE (PROCESSES):
2.) Erosion occurs through:
1. ‘hydraulic action’
β (the force of water compresses air trapped in the bank, creating an explosive blast, causing materials to be dislodged π₯)
2. ‘abrasion’
β (the force of water throws bedload against the banks, wearing them down πͺ¨)
3. ‘solution’
β (acidity in the water dissolves the rocks π§ͺ)
ENDING (FINAL PROCESSES):
3.) Rivers flow fastest on the outside bend
β³ increasing erosive power β‘
(causing undercutting and the formation of river cliffs.)
4.) Rivers flow slowest on the inside bend
β³ leading to deposition β³
5.) HELICOIDAL FLOW πͺ
β transfers sediment
β³ from the river cliffs to river beaches
β in a corkscrew movement.
6.) River cliffs retreat
β³ causing meanders to become more pronounced over time and the neck of the meander to become narrower.
7.) During a flood there is more energy
β³ and the water may cut through the neck π
8.) Deposition seals off the old meander
β³ and over time the abandoned channel may dry up β³