Topic 4 UK Rivers Flashcards
What is discharge
The volume of water flowing in a river at one particular point and time
What is the course
The path of a river as it flows downhill
What are features of the upper course
Steep gradient. V-shaped valley, steep sides, shallow channel
What are features of the middle course
Medium gradient. Valley sides wider, deeper channel
What are features of lower course
Low gradient. Very wide valley, deep channel.
Where does vertical erosion mainly take place
Upper course of the river
Where does lateral erosion commonly occur
Dominant in the middle and lower courses of river
What is traction (transportation)
Large particles are pushed along the river bed by the foce of water
What is suspension (transportation)
Small particles like silt and clay are carried along by the water
What is saltation (transportation)
Pebble-sized particles are bouncing along the river bed by the force of the water
What is solution (transportation)
Solube materials dissolve in the water and are carried along.
What is deposition
When a river drops the eroded material its transporting
What does antecedent conditions mean
Pre-existing conditions
In what course are waterfalls mostly found in
The upper course
How are waterfalls formed
The softer rock is eroded more than the hardrock creating a ‘step’. This gets erodedmore and more until a steep drop is then created. This is called a waterfall. The hardrock is eventually undercut by erosion and collapses. The collapsed rocks are swirled around at the foot of the waterfall and erode the softer rock by abrasion creating a plunge pool. Overtime more undercutting causes the waterfall to retreat leaving a steep-sided gorge
How are interlocking sours created
In the upper course of the river most of the erosion is vertically downwards. The creates steep-sided v-shaped valleys. They arent powerful enough to erode laterally so they have to wind around the valleys. The hillsides that interlock with eachother are called interlocking spurs
What are meanders
Large bends in rivers commonly found in middle to lower courses of the river
Describe the erosion of a meander
The current is faster on the outside of the bend because the river bend is deeper and less friction to slow the water down. Therefore more erosion takes place on the outside of the bend causing river cliffs. The current is slower on the inside of the bend because the river channel is shallower, more friction to slow down water. So eroded material is deposited on the inside of the bend causing slip off slopes
How are ox-bow lakes formed
When meanders get larger over time - they can eventually turn into an ox-bow lake. Erosion causes the outside bend ti get closer until there is only a small bit of land left between the bends. The river breaks through this land. And the river flows along the shortest course. Deposition eventually cuts off the meander creating an ox-bow lake.
What are flood plains
The wide valley floor on either side of a river which ocassionally gets flooded
What are levees
Natural enbankments (raised bits) on the edges of a river channel
How are deltas formed
Rivers are forced to slow down when coming across a sea or lake. This causes them to deposit the material that theyre carrying. The sea doesnt wash it away and this builds up intil low lying areas of land is being built up called deltas
What climates cause a higher discharge
Wetter climates
What does a higher disharge cause
An increased rate of erosion because if w river has a higher volume of water it has more power to erode river banks. Also an increase in transportation as it has more energy to transport material