Linked from

The 9 pages that link to Pore water pressure, each with the reason it gives.

• LandslideRelated: Rising pore pressure can reduce friction and destabilize a slope.

• Debris flowRelated: Rising pore-water pressure reduces grain contact and can help a slope mixture begin flowing.

• Mass wastingRelated: Rising pressure reduces the effective contact forces that hold grains together.

• Slope stabilityRelated: Rising pressure reduces effective stress and can weaken the material along a failure surface.

• Soil liquefactionRelated: Its rapid increase during shaking drives the loss of soil strength.

• Submarine landslideRelated: Rising pore pressure can reduce sediment strength and initiate failure.

• MudflowRelated: Rising pore-water pressure reduces grain-to-grain friction and can destabilize a slope.

• RockslideRelated: Water pressure can reduce frictional resistance along potential failure surfaces.

• Soft-sediment deformation structuresRelated: Changes in this pressure alter sediment strength and can trigger deformation.