The dimensionless parameter describing deformation. It can be thought of as the movement of one corner of a cubic box from its initial position under a stress:
where dl is the change in length and l is the original length. Materials often respond very differently depending on
the rate at which straining occurs
Elasticity, Hooke's Law, Seismic Strain, Strain Rate, Strain Tensor, Strength, Stress
References
Turcotte, D. L. and Schubert, G. "Stress and Strain in Solids." Ch. 2 in Geodynamics: Applications of Continuum Physics to Geological Problems. New York: Wiley, pp. 74-103, 1982.