The Hidden Danger of Coastal Cliffs: How Waves Shape Rocky Slopes

Ever wondered how crashing waves slowly chip away at towering coastal cliffs, eventually causing massive landslides? Let’s dive into the science behind it!

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Published February 26, 2025 By EngiSphere Research Editors

In Brief

This research examines how wave pressure affects the long-term stability of coastal rocky slopes, revealing that flatter slopes experience higher wave-induced stress, which accelerates erosion and increases landslide risks.


In Depth

The Power of Waves: Engineering the Stability of Coastal Rocky Slopes. The Battle Between Land and Sea

Coastal cliffs are breathtaking natural wonders, but beneath their beauty lies a hidden danger: the slow yet relentless impact of waves, tides, and even earthquakes that can weaken rocky slopes over time. As waves pound against these structures, they exert powerful forces that could eventually lead to catastrophic landslides. This is a major concern for coastal infrastructure, tourism hotspots, and marine ecosystems.

A recent study explores how wave pressure affects the long-term stability of coastal rocky slopes, offering new insights into how these formations weaken over time. Let’s break it down! 🏗️⚖️

How Waves Weaken Coastal Slopes
The Science Behind It

Coastal slopes are constantly under attack by dynamic forces such as:

  • Wave impact – Repeated crashing waves create pressure that weakens rock layers.
  • Tides – The constant rise and fall of water levels erode rock surfaces.
  • Seismic activity – Earthquakes add additional stress, making slopes more prone to failure.

Over time, these forces lead to the slow deterioration of weak rock structures. The study found that specific geological features—such as bedding planes and fractures—make some slopes more vulnerable than others.

Simulation and Analysis

To understand these effects, researchers built a geological model of coastal slopes and used computational fluid dynamics (CFD) to simulate wave interactions. The results showed that:

  • Slopes with steeper angles (closer to 90°) experience less wave pressure.
  • Gentler slopes (closer to 30°) absorb more wave force, increasing the risk of erosion and landslides.
  • The relationship between wave pressure, wave height, and slope angle follows an exponential pattern.

In simple terms: flatter coastal slopes take a bigger hit from waves, making them more likely to collapse over time!

Engineering Insights: The Formula for Safety

To calculate the stability of coastal slopes, researchers applied the limit equilibrium method, a technique widely used in geotechnical engineering. They also accounted for the effects of strain-softening, a phenomenon where rock materials lose strength due to repeated stress.

Here’s how stability is assessed:

  1. Measure key rock properties (e.g., friction angle, cohesion, strain-softening behavior).
  2. Analyze wave forces to determine how much shear stress is applied to weak rock layers.
  3. Calculate the Factor of Safety (FOS) – a measure of how stable a slope is over time.
  4. Predict long-term stability – If the stress caused by waves exceeds a critical threshold, the slope will eventually collapse.

A key takeaway? If wave pressure continuously weakens a slope's shear strength, a landslide is just a matter of time.

Future Prospects: Engineering for Coastal Resilience

What can be done to protect coastal cliffs and communities?

Reinforcement Engineering: Installing protective barriers or using retaining structures can help slow down erosion.
Smart Coastal Planning: Avoiding construction near vulnerable cliffs can prevent damage before it happens.
Wave Energy Dissipation: Artificial reefs and submerged barriers can absorb wave energy before it reaches the shore.
Monitoring & Early Warning Systems: Advanced sensors and AI models can predict when a slope is becoming unstable.

With the right engineering approaches, we can mitigate landslide risks and protect both nature and human development.


In Terms

Wave Pressure – The force exerted by ocean waves as they crash against surfaces, gradually wearing them down.

Coastal Rocky Slopes – Steep landforms made of rock that border the ocean, constantly shaped by waves, wind, and tides.

Erosion – The gradual wearing away of rock and soil due to natural forces like wind, water, and waves.

Shear Stress – A force that causes materials (like rock layers) to slide past each other, leading to cracks or collapse.

Strain-Softening – A weakening process where rock or soil loses strength over time due to repeated stress.

Factor of Safety (FOS) – A number used in engineering to measure how stable a structure (like a cliff) is before it fails.

Limit Equilibrium Method – A calculation method engineers use to predict when a slope might become unstable and collapse.


Source

Sun, M.; Shan, Z.; Wu, H.; Liu, Q.; Wang, J. Long-Term Stability Evaluation Method of Coastal Rocky Slope Considering Wave Loading. Water 2025, 17, 637. https://doi.org/10.3390/w17050637

From: PowerChina Huadong Engineering Corporation Limited; China University of Geosciences.

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