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Understanding Mohr-Coulomb Failure Criteria in Rock Mechanics

A fundamental principle for predicting when rocks will fail under stress.

mysimulator teamUpdated June 2026≈ 4 min read▶ Open the simulation

What is the Mohr-Coulomb Theory?

The Mohr-Coulomb theory is a widely used model in rock mechanics to predict when rocks will fail under stress. It describes how shear stress (τ) and normal stress (σ) interact within materials, particularly rocks, to determine their strength. The theory was developed by Adhémar Jean Claude Barré de Saint-Venant and later refined by Hubert Henry Mohr and André Coulomb.

The key idea is that the material will fail when the shear stress acting on a plane exceeds the maximum shear stress (τ_max) that can be supported by the normal stress (σ_n) and cohesion (c). This relationship is described by the equation: τ = c + σ_n * tan(φ), where φ is the friction angle of the material.

How Does It Work?

The Mohr-Coulomb theory operates on a stress circle, or Mohr circle, which visualizes the state of stress at any point within a rock. The horizontal axis represents normal stress (σ), and the vertical axis represents shear stress (τ). As you rotate a candidate fracture plane through this stressed rock block, the Mohr circle dynamically updates to show how these stresses change.

The theory predicts that failure occurs when the applied shear stress exceeds the frictional strength of the material. This is represented by the angle at which the normal stress and shear stress intersect on the Mohr circle, known as the Coulomb angle.

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Why Does It Matter?

Understanding the Mohr-Coulomb theory is crucial for predicting landslides, earthquakes, and other geological hazards. Engineers use this knowledge to design stable structures such as dams, tunnels, and foundations that can withstand the forces exerted by rock masses.

In mining operations, it helps in planning safe extraction methods and preventing cave-ins or collapses of mine walls.

Real-World Applications

The Mohr-Coulomb theory is applied in various fields including civil engineering, geotechnical engineering, and petroleum engineering. For instance, it aids in the design of retaining walls that prevent soil movement, ensuring safety in construction projects.

In mining, engineers use this principle to predict potential failure points in rock formations, helping to avoid catastrophic collapses.

Frequently asked questions

How does cohesion (c) affect the Mohr-Coulomb failure criterion?

Cohesion represents the internal frictional resistance between particles within a material. A higher cohesion value means that more shear stress is required to initiate failure, shifting the Coulomb line on the Mohr circle upwards.

Can the Mohr-Coulomb theory be used for all types of rocks?

While the theory provides a good approximation for many rock types, its accuracy can vary depending on the specific properties of the material. For highly anisotropic or heterogeneous rocks, more complex models may be necessary.

What is the significance of the friction angle (φ) in Mohr-Coulomb theory?

The friction angle represents the internal friction between particles within a rock mass. It determines how easily the material can slide against itself, with higher angles indicating greater resistance to sliding.

How does the stress state of rocks change during an earthquake?

During an earthquake, the stress state in rocks changes dramatically as tectonic plates move and interact. The sudden release of energy can cause a shift in the Mohr circle, potentially leading to failure along fault lines if the new stress state exceeds the material's strength according to the Mohr-Coulomb criterion.

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Everything above runs in your browser — open Mohr-Coulomb Faulting Simulator and change the parameters while it is running. Nothing is installed, nothing is uploaded, the whole model lives in one tab.

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