Valleys eroded due to fast flowing water often found in upland areas
V shaped valley formation
river erodes vertically down and it leaves behind valley sides shaped like a V
because as it erodes straight down it leaves very steep valley sides
that are then attacked by weathering processes such as freeze thaw and biological weathering.
This weakens the valley sides which may collapse or move down slope due to mass movement processes such as slumping
The river can then erode this material and move it away, leaving behind the characteristic V shape.
Interlocking spurs
series of ridges projecting out on alternate sides of a valley and around which a river winds its course.
Interlocking spurs formation
upper course of a river most erosion is vertically downwards. This creates steep sided, V shaped valleys
The rivers aren't powerful enough to erode laterally (sideways) - they have to wind around the high hillsides that stick out into their paths on either side
hillsides that interlock with each other as the river winds around them are called interlocking spurs
Dams and reservoirs description
A ealk built across a river which majes an artificial lake called a reservoir
The environmental agency monitors rivers and issues warnings via newspapers, TV, radio and the internet when they are likely to flood so people can prepare.
Restoring rivers to more natural course by taking away embankments and restoring meanders. This allows rivers to flood but slows them down. However you may still need flood banks.