Erosion in the upper course
Hydraulic action and attrition. Mostly vertical erosion
Erosion in the middle course
Mostly attrition and a little hydraulic action. Less vertical erosion, lateral erosion begins
Erosion in the lower course
Erosion is reduced some lateral erosion on the outside bends of rivers
Transport in the upper course
Mostly large boulders, little in solution. Traction is most dominant
Transport in the middle course
Smaller sized bedload little in solution. Saltation dominated
Transport in lower course
Smaller sized bedload of pebbles, gravel and sand for the load. Most transport by suspension
Deposition in the upper course
Limited due to large bedload
Deposition in the middle course
Coarser material builds up, deposition on slip off slopes. Floodplain build up in times of flood
Deposition in lower course
Mostly fine particles, forms slip off slopes, leeves and flood plains
Gradient in upper course
Steep
Gradient in middle course
Less steep
Gradient in lower course
Grendel gradient/ flat
Associated landforms in the upper course
Steeped narrow, v shaped valley, waterfalls/ Rapids, interlocking spurs
Associated landforms in the middle course
Open v- shaped valley, waterfalls/Rapids, meanders/ox bow lakes, braiding
Assassinated landforms in the lower course
Wide gentle sided valley, flood plains, knick points, leeves, river terraces, meanders, ox bow lakes braiding
How is a waterfall formed
When a river passes over harder rock (wintstone) which is on top of softer rock, the softer rock is eroded faster by abrasion and hydraulic action. This creates and overhang and cracks appear in the wintstone. The overhang collapses and the wintstone fills in the plunge pool. This process continues to happen and the waterfall retreats upstream and forms a steep sided gorge
In the middle course, why does the river have more energy and a high volume of water
Because the tributaries have joined and there is more water from through-flow and surface runoff.
How is a levee formed
During floods water is slowed at banks and silts are deposited. In between floods slow moving water deposits silt in water bed. The levees are built up with each flood and the river bed is built up too. The amount of water stays the same
Wheat is an estuary
An area where fresh water, river or stream meets the ocean, this results in brackish, somewhat salty water
Characteristics of a flashy response river
Short lag time, steep rising and falling limb, returns to normal quickly, high peak discharge, most likely to cause flood
What causes a flashy response
Basin with impermeable rock- flows after over ground
Urbanised catchment- artificial drains and tarmac so water will flow faster
Basin with steep sides- water will flow faster
Short heavy rainfall
Characteristics of a slow response
Long lag time, low peak discharge, gentle rising and falling limbs, returns to normal slowly, less likely to cause a flood
What causes a slow response
A forested catchment- more interception
Has a dam- slows down the flow
Shallow sided basin- more water is absorbed into the ground
Basin with permeable rock
Human causes of flooding
Deforestation
Construction work