3.3 Slope processes Flashcards
1
Q
Explain how slopes vary with climate
A
- In humid and wet areas slopes are rounder, due to chemical weathering, soil creep and fluvial transport
- In contrast, in arid/dry regions, slopes are jacked or straight owing to mechanical weathering and sheetwash
2
Q
Explain how geological structure affects slopes
A
- This includes faults, angle of dip and vulcanicity - these factors influence the stength of a rock and create lines of potential weakness within it
- Rock type and character affects vulnerability to weathering and the degree of resistance to downslope movement
- Slopes composed of many different types of rock are more vulnerable to landslides due to different types of erosion
3
Q
Explain how soil affects slopes
A
- Structure and texture determine how much water it can hold
- Clay soils can hold more than sandy soils
4
Q
Explain how aspect affects slopes
A
- South facing slopes can be more exposed to freeze thaw due to large variations in temperature
- Can be exposed to more heat causing more heating and cooling
5
Q
Explain how vegetation affects slopes
A
- Vegetation can decrease overland runoff through the interception and storage of moisture
- Deforested slopes are exposed to intense erosion and weathering
- However, vegetation can increase the chance of major landslips - dense forest reduce surface wash, casuing a build up of soil, increasing the potential for failure
6
Q
How can slopes be classified
A
- Speed of movement
- Water content
- Type of movement - flows, slides, slumps
- Material
7
Q
What causes mass movements/slope failure
A
- Gravity, slope angle and pore pressure
- A reduction in internal resistance i.e. shear strenght
- An increase in shear stress - forces attempting to pull a mass downslope
- When shear stress is greater than shear strength, the slope fails
- Loose rock, stones and soil all have a tendency to move downslope - THEY DO SO WHENEVER THE DOWNWARD FORCE EXCEEDS THE RESISTANCE PRODUCED FRICTION AND COHESION
8
Q
Explain the role of water in mass movement
A
- It can increase the shear stress or decrease the shear stress through
- Water increases the lubrication which reduces the friction between the sliding surfaces
- It may increase the weight of the soil
- Pressure from pore water is increased which reduces the strength allowing movement to take place e.g mudflows
- Wetting and drying of soils may lead to soil heave and creep
- Freeze thaw in joints on rock cliffs may lead to rockfall
9
Q
Describe and explain the process of heave/creep
A
- Slow, small scale movement of soil down shallop slope gradients (2 cm per year)
- Talus creep is the slow movement of fragments on a scree slope
- Heave involves repeated lifting and settling of particles making up the soil THROUGH WETTING AND DRYING OR FREEZE THAW
10
Q
Describe and explain the process of slumps
A
- Slow to rapid downslope movement of earth material along a CURVED SLIP PLNE as a unit
- Usually occurs in weak materials such as clay after it absorbs water and becomes saturated
- Often the strength is reduced due to the undercutting of the base of the cliff
11
Q
Describe and explain flows
A
- Flows are more rapid, continuous and less jerky mass movements
- The speed of a flow varies - mudflows are faster and more fluid than earthflows
- More water allows flows over more shallow slopes
12
Q
Describe and explain slides
A
- Slow to rapid downslope movement of larrge units of rock along a slip plane
- Occur due to weak rocks, steep slopes and active undercutting of the cliff
- Loose rock, stones and soil all have a tendency to move downslope - THEY DO SO WHENEVER THE DOWNWARD FORCE EXCEEDS THE RESISTANCE PRODUCED FRICTION AND COHESION i.e. shear stress is greater than shear strength
13
Q
Describe and explain the process of falls
A
- They occur on steep slopes especially on bare rock faces where joints are exposed
- The initial cause of the fall may be weathering, such freeze-thaw or disintegration, or erosion prising open lines of weakness
- Once rocks are detached they fall under the influence of gravity largely through the air
14
Q
Describe and explain surface wash
A
- This occurs when the soil’s infiltration capacity is exceeded
- In the UK, this occurs in winter when the ground is frozen and water cannot seep through
- Can occur after heavy rainfall or when snow melts
15
Q
Describe and explain sheetwash
A
- Unchannelled flow of water over a soil surface
- On most slopes, sheetwash breaks into areas of high velocity separated by areas of low velocity
- It occurs on footpaths and moorlands
- It can result in a uniform layer of soil being eroded - it occurs through raindrop impact and subsequent transport by water flowing overland rather than in channels