Linked from

The 17 pages that link to Slope stability, each with the reason it gives.

• LandslideRelated: A landslide begins when driving forces overcome the slope's resistance.

• Geotechnical engineeringBroader topic: Geotechnical analysis identifies failure surfaces and evaluates stabilizing measures.

• Effective stressRelated: Rising pore pressure lowers effective stress and can reduce resistance to sliding.

• Mass wastingRelated: Mass wasting begins when a slope loses this balance.

• Angle of reposeNarrower topic: Repose angle concerns loose piles; slope stability addresses broader terrain and engineered slopes.

• Soil mechanicsRelated: Soil strength, groundwater, and loading determine the likelihood of slope movement.

• Columnar jointingRelated: Joint orientations can define blocks that affect failure modes in columnar cliffs.

• Strike and dipRelated: Rock-plane orientations help assess whether discontinuities can daylight into a slope.

• Pore water pressureRelated: Rising pore pressure can lower effective stress and trigger slope failure.

• EarthworksRelated: Excavation and embankment change slope geometry and can trigger failure.

• Mohr–Coulomb theoryRelated: The criterion estimates shear resistance along potential slip surfaces in soil and rock.

• Pore waterRelated: Changes in pore pressure can weaken slopes and promote landslides.

• Dam safetyRelated: Unstable embankments and abutments can threaten a dam or its reservoir margins.

• MudflowRelated: Failure of slope stability can release the saturated material that forms a mudflow.

• RockslideNarrower topic: Rockslide hazard depends on whether the slope remains in mechanical equilibrium.

• GeomechanicsRelated: Geomechanical strength and groundwater conditions determine whether slopes remain stable.

• MudrockRelated: Water-sensitive mudrock can weaken and contribute to landslides and slope failure.