topic 4 - river landscape Flashcards
the upper course
gradient -
valley and channel shape
steep gradient
the valleys are steep-sided and shaped like a v
water flows through a narrow and shallow channel
In the upper course,
erosion
erosion dominates over the deposition
the middle course
gradient -
valley and channel shape-
medium gradient
valleys have a gentle slope
wider and deeper channel than the upper course
the lower course
gradient -
valley and channel shape
gentle gradient
very wide and flat valley sides
the channel is wide and deep
cross
profile
shows you what a cross-section of the river looks like.
long
profile
Shows you how the gradient of a river changes along its length.
Types of River Erosion
vertical erosion
lateral erosion
lateral erosion
lateral erosion makes the river valley wider
lateral erosion dominated in the middle and lower Course
vertical erosion
vertical erosion makes the river valley deeper
vertical erosion dominates the upper course
due to high turbulence causing the rough and angular particles to be scrapped along the river bed
processes of transportation
solution
traction
saltation
suspension
process of erosion
hydraulic action
abrasion
attrition
solution
solution
soluble material dissolved in the water and are carried along
suspension
small particles like slit and clay are carried along by the water
saltation
when small particles bounce along the river bed by the force of the water
traction
is where large panicles eg boulders are dragged along the river bed by the force of the water
disposition is when a river drops eroded material
4 reasons why rivers slow down and deposit material
the water becomes shallow
the river reaches the mouth
reduced volume of water in the channel
the number of sediments in the channel increases