Eden Basin Flashcards
1
Q
Location of the Eden Basin:
A
- North-West England, between mountains of the Lake District and the Pennines
- The source is in the Pennine hills in South Cumbria
- It is largely a rural area, with many scenic landscapes popular with tourists
2
Q
How was Hell Gill Force-waterfall formed?
A
- Near the source of the River Eden
- It has formed where there it has changed from hard limestone to soft sandstone.
- Eroded the soft rock, forming a step.
- As the waterfall as retreated up the valley it has left behind a steep-sided gorge.
3
Q
How are meanders formed?
A
- When tributaries join the Eden, the river gets bigger, more power to erode the river channel sideways.
- In the lower course, the river valley becomes wider and flatter and meanders form near Salkeld
- They have been cut off to form ox-bow lakes. Where Briggle Beck joins the Eden
4
Q
What is the climate of the Eden Basin?
A
- Cumbria faces the prevailing south-westerly winds
- Mild and wet
- Cool summers and mild winters.
5
Q
How are geomorphic processes influenced by temperature?
A
- During cold periods, FTW can slowly break up the exposed rock of the valley sides in the upper course
- The sides are weakened, makes mass movement is more likely
- Adds to the river’s load increasing erosive power through abrasion.
6
Q
How does rainfall impact geomorphic processes?
A
- Ground becomes saturated, heavier, less stable, river banks slump
- Heavy rain can flow quickly into the river, volume of water rapidly increases
- Increases transportation which causes more erosion by abrasion.
7
Q
How do igneous rocks influenced the geomorphic processes?
A
- Found in the west of the Eden Basin, tend to be impermeable
- High rainfall causes lots of surface streams to form
- Have a lot of power to erode vertically, creating steep-sided V-shaped valleys.
8
Q
How do softer rocks influenced the geomorphic processes?
A
- Middle and lower courses is made up of sandstone
- Increasing volume of the river, leads to lots of lateral erosion
- This widens the river channel and forms meanders and steep river cliffs.
9
Q
How does deforestation impact geomorphic processes?
A
- Natural woodland and heathland have been cleared from upland areas
- Increases surface runoff when it rains
- More water ends up in river channels more quickly
- More energy for erosion, causes sliding and slumping of the river banks.
10
Q
How does farming impact geomorphic processes?
A
- Some upland areas have been drained of moisture to make them suitable for farming
- Reduces stability of soil, more soil in the channel
- Increased load, increases deposition
- Changing the floodplain landscape from its natural state.
11
Q
How have flood walls and embankments influenced it?
A
- 10km of raised flood defences have been built along the River Eden and Caldew
- Designed to contain the water in the river, so that the floodplain can be built on
- Interrupt natural processes of the river, can prevent natural formation of meanders and deposition of sediment on the floodplain.
12
Q
How does planting trees influence it?
A
- Near Dalston, 1000 trees have been planted to reduce flooding and erosion by stabilising the soil
- Trees intercept rainfall, reduce surface runoff, prevents rapid increases of volume of water
- Less energy for river, reducing lateral and vertical erosion
- Meanders take longer to form.