As an important application of the theory of elasticity in soil mechanics, the main principles of elastodynamics are introduced. On the basis of waves in 1D-continua the notions of transmission, reflexion and dynamic stiffness are explained, and the body waves are presented as compression and shear waves. Rayleigh waves are presented as an example of surface waves.

When the mass balance on a glacier changes, the glacier is prone to either advance or retreat. A number of feedback processes can amplify or suppress the reaction. During the Pleistocene, ice sheets fluctuated in phase with the concentration of greenhouse gases in the atmosphere, but which forced the other is uncertain. Changes in mass balance result in a stable response in accumulation areas and an unstable response in ablation areas. In the latter, stability is restored by the arrival of a kinematic wave from the vicinity of the equilibrium line. Kinematic waves on glaciers move as several times the speed of the ice as a whole, and are subtle in topographic expression. For small perturbations, the response time of a glacier to a perturbation in mass balance can be estimated by dividing the maximum thickness of the glacier by the balance rate at the terminus. This estimate can be improved by taking into consideration the lag between the time the perturbation is felt in the accumulation area and the time necessary to transmit that signal to the terminus.