Landslides are one of the most destructive natural disasters seen across the world — especially in hilly regions like Sri Lanka, India, Nepal, Japan, and many mountainous countries. Every year, hundreds of homes, roads, bridges, and farms are damaged due to slope failures. But what actually causes a landslide?
From a civil engineering perspective, the answer is a combination of soil behaviour, groundwater movement, slope geometry, weather, and human activity.
In this article, we break it down in the simplest way possible so that anyone can understand — even without engineering background. Let’s dive in! π
π§± 1. Weak Soil or Rock Layers (Poor Geological Conditions)
One of the biggest reasons slopes fail is the type of soil or rock beneath them. Every soil type has different strength properties — like cohesion, friction angle, and shear strength.
π Weak soils include:
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π€ Soft clay
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π«️ Loose sand
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π Residual soils formed from decayed rock
When these soils absorb water, they lose strength — just like wet sand collapsing under your feet. In civil engineering terms, we call this loss of shear strength, and it is one of the major triggers of landslides.
Why it happens:
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Long-term weathering breaks rock into weak particles
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Areas with old landslides have already disturbed soil
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Poorly compacted fill soil (from construction) settles unevenly
Simple example:
Try building a sandcastle with overly wet or overly dry sand — it collapses. The same thing happens on hillsides.
π§️ 2. Heavy Rainfall & Water Pressure Build-Up
Rainwater is the number one cause of most landslides in tropical countries.
When soil becomes saturated, water fills the gaps between particles, increasing pore water pressure.
⚙️ What does this mean in civil engineering?
Increasing water pressure = decreasing soil strength.
The slope becomes heavier, weaker, and can no longer support itself.
Rain causes landslides through:
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Infiltration of water into the soil
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Rising groundwater table
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Softening clay layers
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Increasing weight of soil
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Washing away the slope (erosion)
Easy explanation:
Think of a sponge. When dry, it's stiff. When filled with water, it becomes soft and collapses easily.
That’s exactly what happens to a hillside terrace or natural slope during intense rainfall.
π 3. Human Activities & Construction Without Proper Engineering
Humans often accelerate natural disasters through unplanned development.
Civil engineers call this anthropogenic causes.
Common mistakes include:
Why it is dangerous:
Cutting a hill removes the original support.
Filling a valley adds extra load on soft soil.
Altering natural drainage sends water into unstable areas.
Civil engineers design slopes using factor of safety (FOS) to ensure stability.
When construction happens without engineering expertise, slopes fail easily.
πͺ΅π² 4. Deforestation & Loss of Vegetation Cover
Trees and plants are nature’s own retaining structures! π±
Their roots:
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Bind soil together
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Reduce erosion
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Absorb large amounts of rainwater
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Anchor soil to bedrock
When forests are cleared:
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Soil loses reinforcement
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Rainwater flows directly into the slope
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Surface erosion increases
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Water infiltration increases
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The slope becomes unstable
Simple comparison:
Grass is like the “glue” for soil.
Removing it makes the soil free to slide.
This is why areas with landslides often show:
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Recent land clearing
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Tea plantation expansions
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Illegal timber cutting
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Shifting cultivation
π 5. Earthquakes & Vibrations
Earthquakes shake the ground and reduce soil strength instantly.
In engineering terms:
Earthquake waves = increased shear stress
Loose soil (especially sand) = loss of friction
Steep slopes = rapid movement
Even small vibrations from heavy trucks or blasting can trigger a landslide in weak soil.
Critical risk zones:
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Mountain roads
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Quarry sites
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Slopes with loose fill material
Earthquake-induced landslides are common in Japan, China, and Nepal — but Sri Lanka has experienced some during minor tremors too.
π§ 6. Poor Drainage (Surface & Subsurface)
Even if the soil is strong, water can destroy it if it has nowhere to go.
Poor drainage causes:
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Water accumulation
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Increased pore water pressure
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Erosion at slope toes
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Softening of soil layers
Civil engineering solutions include:
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Weep holes
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Drainage paths
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Berm drains
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Subsoil drains (French drains)
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Proper road shoulder drains
But when these systems clog or do not exist, slopes fail naturally.
Simple Example:
If a flower pot has no hole at the bottom, the soil becomes soggy.
Slopes behave exactly like that.
π€️ 7. Natural Erosion Over Time
Rivers, streams, and rainwater slowly erode the base (toe) of a slope.
When the toe weakens, the upper soil loses support and collapses.
Causes:
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Riverbank erosion
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Wave action near coastal slopes
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Continuous rainfall runoff
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Poorly managed water channels
As civil engineers, we call this toe failure — a major reason for roadside landslides.
π§ π‘️ 8. Weathering, Climate Change & Long-Term Soil Degradation
Climate plays a huge role in slope stability.
High temperatures, alternating wet and dry seasons, and freezing in some countries all weaken rock.
Over time:
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Rocks break into smaller particles
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Clay minerals form
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Cracks appear
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Soil structure becomes loose
Climate change intensifies rainfall patterns, causing:
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Sudden heavy downpours
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Extended wet seasons
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Unpredictable storms
This increases landslide frequency worldwide.
π ️ 9. Poorly Designed Retaining Structures
Not all retaining walls are engineered correctly.
Common problems:
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No weep holes
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No filter material
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Poor backfilling
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Insufficient foundation depth
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No reinforcement
When water builds up behind a poorly designed wall, the pressure becomes too high, causing the wall to tilt or collapse — triggering a landslide above or below it.
A retaining wall without drainage = a disaster waiting to happen.
π£️ 10. Road Cutting, Tunneling & Infrastructure Works
Roads built along hillsides require careful slope stabilization.
Mistakes include:
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Cutting slopes at nearly vertical angles
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Not protecting slopes with shotcrete
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No gabion walls or geotextiles
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Daylight cuts exposing weak soil
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Vibrations from heavy machines
Similarly, tunneling or blasting disturbs deep soil layers, creating fractures that later become sliding surfaces.
π§ͺ 11. Failure of Fill Slopes & Embankments
Construction projects often require filling to raise land levels.
But fill material must be:
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Properly compacted
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Layered correctly
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Tested for density
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Free of organic matter
Improperly compacted soil settles unevenly, absorbs water quickly, and becomes heavy — causing deep-seated failures.
This is a common problem in:
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Highway embankments
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Housing schemes
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Agricultural terraces
π️ 12. Natural Slope Geometry – Too Steep, Too High, Too Weak
Even without rainfall or human activity, some slopes are naturally unstable.
Factors include:
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Height of the slope
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Angle of inclination
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Depth of weathering
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Type of rock
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Pre-existing cracks
Civil engineers measure stability using:
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Slope angle (ΞΈ)
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Cohesion (C)
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Friction angle (Ο)
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Unit weight (Ξ³)
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Factor of safety (FOS)
If the FOS is below 1.5 (recommended), the slope is unsafe.
π Summary: What Really Causes Landslides?
✔️ Natural Causes
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Heavy rainfall
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Weak soil
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Earthquakes
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Weathering
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Natural erosion
✔️ Human Causes
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Deforestation
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Unplanned construction
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Bad road cutting
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Poor drainage
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Excessive load on slopes
✔️ Engineering Causes
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Wrong retaining wall design
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Improper fill compaction
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Poor slope stabilization
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Disturbance of slope toe
A landslide usually occurs due to a combination of several causes, not just one.
π How We Can Prevent Landslides (Simple Methods)
π± 1. Plant more trees & avoid clearing hillsides
Roots strengthen soil naturally.
π§ 2. Build proper retaining walls & provide drainage
Drainage is the key to slope stability.
π£️ 3. Avoid steep slope cutting
Always follow recommended safe angles.
π§️ 4. Maintain road drains & water paths
Keep water flowing away from the slope.
π§± 5. Follow engineering guidelines for fill construction
Compaction is critical.
π§ 6. Get geotechnical investigations before building
Soil tests reduce disaster risks.

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