Why do slopes fail, and how can landslide hazards be reduced?
Mass movement is the downslope movement of rock and soil under gravity; it includes slow creep, slides, slumps, flows and rockfalls; failure is triggered when the driving force (gravity, increased by steep slopes, heavy rain, loading and undercutting) exceeds the resisting force (friction and cohesion, reduced by water and weak or weathered rock); the risk is reduced by improving drainage, reducing slope angle, building retaining structures and avoiding building on unstable ground.
A focused answer to the Eduqas GCSE Geology statement on mass movement. Covers the types of mass movement, why slopes fail (the balance of driving and resisting forces and the role of water), the triggers, and how landslide risk is reduced by drainage, regrading, retaining structures and avoidance.
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What this dot point is asking
Eduqas wants you to explain mass movement, the downslope movement of rock and soil under gravity, to name its types (creep, slides, slumps, flows and rockfalls), and to explain why slopes fail using the balance between the driving force (gravity, raised by steep slopes, heavy rain, loading and undercutting) and the resisting force (friction and cohesion, lowered by water and weak rock). You also need to explain how risk is reduced (drainage, reducing slope angle, retaining structures, and avoiding unstable ground). The high-mark questions ask you to apply the force balance, especially the role of water.
The answer
What mass movement is
Mass movement is the movement of rock and soil downslope under gravity. It ranges from imperceptibly slow to catastrophically fast:
- Creep. Very slow, continuous movement of soil downhill (millimetres a year), shown by tilted fences and curved tree trunks.
- Slides. A mass moves down a flat or planar surface, keeping much of its shape (a landslide).
- Slumps. A mass rotates along a curved surface, so the top tilts back (common in clay cliffs).
- Flows. Saturated material flows like a fluid (mudflows and earthflows).
- Rockfalls. Blocks detach from a cliff and fall or bounce down.
Why slopes fail: the force balance
Whether a slope holds or fails comes down to two opposing forces:
- The driving force is the downslope pull of gravity. It is larger on steeper slopes, when extra weight is added (rain, buildings, spoil), and when the base is undercut.
- The resisting force is the friction and cohesion holding the material in place. It is smaller in weak, weathered or clay-rich rock and when water is present.
A slope is stable while the resisting force is greater than the driving force, and it fails when the driving force exceeds the resisting force.
The triggers (especially water)
A slope near the balance can be tipped into failure by a trigger:
- Heavy rain. Water does two things at once: it adds weight (raising the driving force) and it lubricates the grains and raises pore-water pressure (pushing grains apart and lowering friction and cohesion, so the resisting force falls). This is why so many landslides follow heavy rain.
- Steepening or undercutting. Waves at a cliff base, or a road cut, remove support and steepen the slope, raising the driving force.
- Loading. Buildings or spoil tips add weight to the top of a slope.
- Earthquakes. Shaking can trigger slides and rockfalls directly.
- Weak or weathered rock. Clay and heavily weathered rock have low strength, so the resisting force is low to begin with.
Reducing the risk
Engineering measures work by lowering the driving force or raising the resisting force:
- Improve drainage. Drains and pipes remove water, cutting the weight and restoring friction and cohesion. Often the most effective single measure, because water is the usual culprit.
- Reduce the slope angle (regrade). Cutting the slope back, or terracing it, lowers the downslope component of gravity.
- Retaining structures. Walls, rock bolts, gabions and netting physically hold material back, adding to the resisting force.
- Vegetation. Plant roots bind soil and take up water.
- Avoid building on unstable ground. Hazard mapping identifies slopes likely to fail so development can be sited elsewhere.
Examples in context
Example 1. Coastal clay cliffs. Soft clay cliffs slump repeatedly because clay is weak when wet and waves keep undercutting the base. Drainage and sea defences at the toe are the usual response.
Example 2. Creep on a hillside. Slow soil creep is harmless to people but tilts fence posts and walls and curves tree trunks over years, a reminder that gravity acts on every slope, not just the steep ones.
Try this
Q1. Name the force that drives mass movement. [1 mark]
- Cue. Gravity (the downslope component of gravity, the driving force).
Q2. Explain why heavy rain makes a slope more likely to fail. [2 marks]
- Cue. Water adds weight (increasing the driving force) and lubricates the grains and raises pore-water pressure (reducing friction and cohesion, the resisting force).
Q3. Give one engineering measure that reduces the risk of mass movement and how it works. [2 marks]
- Cue. For example improving drainage (removes water, lowering weight and raising friction), or reducing the slope angle (lowers the downslope pull of gravity).
Exam-style practice questions
Practice questions written in the style of WJEC Eduqas exam questions on this dot point, with worked answer explainers. The year tag is the paper they imitate, not the source.
Eduqas 20216 marksExplain why a coastal slope of clay becomes more likely to fail after a period of heavy rain, using the idea of driving and resisting forces.Show worked answer →
Frame failure as driving force versus resisting force, then show how rain shifts the balance.
- The balance that holds a slope
- A slope is stable while the resisting force (friction and cohesion holding the material in place) is greater than the driving force (the downslope pull of gravity). Failure happens when the driving force exceeds the resisting force.
- How rain raises the driving force
- Water soaking into the clay adds weight to the slope, increasing the downslope driving force.
- How rain reduces the resisting force
- Water lubricates the grains and raises the water pressure in the pores, which pushes the grains apart and reduces friction and cohesion. Wet clay is weak and slippery, so its resisting force falls.
- The result
- Heavy rain increases the driving force and decreases the resisting force at the same time, so the slope is far more likely to fail. (Wave undercutting at the base also removes support.)
Markers reward the driving-versus-resisting framework and the point that water both adds weight (more driving force) and lubricates and raises pore pressure (less resisting force), so failure becomes likely.
Eduqas 20194 marksA housing development is planned on a steep slope of weathered rock. Suggest two engineering measures that could reduce the risk of mass movement, and explain how each works.Show worked answer →
Give two valid measures, each with the mechanism by which it stabilises the slope.
- Improve drainage
- Installing drains or drainage pipes removes water from the slope. This lowers the weight (driving force) and raises friction and cohesion (resisting force), because dry material is stronger and less lubricated.
- Reduce the slope angle (regrading)
- Cutting the slope back to a gentler angle reduces the downslope component of gravity (the driving force), making the slope more stable. Building it in benches or terraces has the same effect.
- Retaining structures
- A retaining wall, rock bolts or wire netting physically hold the material back, adding to the resisting force. (Planting vegetation to bind the soil with roots is also valid.)
Markers reward two distinct measures, each explained by how it lowers the driving force or raises the resisting force.
Related dot points
- Earthquakes are caused by the sudden release of stress along faults, mainly at plate margins; they radiate seismic waves (P-waves and S-waves) whose arrival times locate the epicentre and whose amplitude measures magnitude; the hazards include ground shaking, building collapse, tsunamis, fires and landslides; the risk is reduced by hazard mapping, building design and emergency planning, but precise short-term prediction remains impossible, so forecasting relies on probability from past records.
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- Engineering geology assesses the ground before construction: foundations, tunnels, dams and reservoirs must suit the rock and soil present; geologists check the strength and stability of rock, the presence of faults, the slope stability, the permeability of the ground (for a reservoir to hold water or a tunnel to stay dry), and the hazards of weak, soluble or swelling materials; poor ground investigation can lead to subsidence, leakage, collapse or failure, so a site investigation is carried out first.
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- Hydrocarbons (oil and gas) form from buried organic matter, then migrate from a source rock into a porous, permeable reservoir rock where an impermeable cap rock and a trap (for example an anticline or fault) hold them; groundwater is stored in a porous, permeable aquifer beneath the water table and supplied to wells; both depend on the rock properties porosity (storage) and permeability (flow), and both can be over-exploited or polluted.
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Sources & how we know this
- WJEC Eduqas GCSE (9-1) Geology specification (teaching from 2017) — WJEC Eduqas (2017)