P1: Rivers Flashcards
long profile
How the Steepness of the River changes from source to mouth.
Upper course - steep
Middle course - shallow
Lower course - almost flat near the mouth
Cross profile
How the river and its valley change shape.
Upper course - V - shaped valley
Middle - sloped hills and shallow river
Lower course - Flat sides and deep river.
Vertical erosion
Happens in the upper course
Lateral erosion
In the lower course because the gradient is lower.
Attrition
The load collides into each other and becomes smaller fragments
Solution
Water dissolves certain rocks
Hydraulic action
Water forces air into crack which then explode under pressure.
Abrasion
The process of scraping or wearing something away
Traction
large boulders are rolled
saltation
The bouncing of sediment
suspension
fine clay and sediment is lifted and carried
Deposition
When sediment can not be carried anymore by the river because the energy drops leading to the sediment being dropped on the riverbed.
Interlocking spurs
Occurs where there are bands of resistant and less resistant rock. Vertical erosion is high as there is a steep gradient so it cuts out a v- shaped valley. Weathering wears the valley sides. River winds around the more resistant rock
Rapids
vertical bedding- differential erosion.
There is turbulent flow on the steps.
Waterfall / gorge
Vertical bedding - vertical erosion is dominant.
differential erosion happens by abrasion and hydraulic action forms rapids.
Undercutting occurs - because splash back happens where the most turbulent flow is. Creates an overhang. A plunge pool forms. Gravity causes the cap rock to collapse. This makes the plunge pool deeper.