Linked from

The 15 pages that link to Creep (deformation), each with the reason it gives.

• ViscoelasticityRelated: It shows how viscoelastic materials continue deforming while a load remains constant.

• RheologyRelated: Creep tests reveal how deformation changes over time under constant load.

• Plastic deformationCompared with: Creep can accumulate permanent strain even when stress remains below short-term yield strength.

• RefractoryRelated: Long-term creep can distort a lining even when it remains below its melting point.

• Ligament (anatomy)Related: Ligaments can lengthen over time when sustained forces exceed their usual demands.

• Polycrystalline materialRelated: Grain-boundary processes can control creep in polycrystals.

• Mantle viscosityNarrower topic: Mantle flow is creep through crystalline rock rather than motion of a liquid.

• Piezoelectric actuatorRelated: After a voltage step, piezoelectric actuators can continue drifting as their material relaxes.

• Pressure solutionNarrower topic: Pressure solution is a chemical mass-transfer mechanism of rock creep.

• Vacancy defectRelated: Vacancy diffusion enables atomic rearrangements involved in high-temperature creep.

• Expansion jointRelated: Long-term deformation can contribute to movement demands at structural gaps.

• Crystallographic defectRelated: Defect motion and diffusion enable slow deformation in crystalline materials.

• PolyoxymethyleneRelated: POM components under constant load must be designed for time-dependent deformation.

• RockslideCompared with: Rockslides are rapid failures, unlike the gradual movement characteristic of slope creep.

• Time–temperature superpositionRelated: Creep compliance measurements can form a master curve using the same shifting principle.