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
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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
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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
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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
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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
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6
Q

How can slopes be classified

A
  • Speed of movement
  • Water content
  • Type of movement - flows, slides, slumps
  • Material
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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
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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
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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
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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
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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
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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
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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
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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
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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
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16
Q

Describe and explain what rills are

A
  • A relatively shallow channel, generally less than tens of cenimetres deep
  • They carry water and sediment for only a short period of time
  • Common in agricultural areas, areas of deforestation or land-use changes
  • Throughflow is water moving through channels in the soil and can transport material
17
Q

Describe and explain rainsplash erosion

A
  • Erosion on hillslopes - when the rain droplet hits the surface it dislodges particles in all directions
  • On 5º slope 60% of movement is downslope
  • This figure increases to around 95% on a 25º slope
  • The amount of erosion depends on rainfall intensity, velocity and rainfall distribution
  • Most effective at the start of a rainfall event when the soil is still loose