Geophysical logs show the seismology data of elastic waves, mainly seismic reflection.

P-waves are a type of elastic wave, called seismic waves in seismology, that can travel through a continuum.

In the case of the earth's inner core, the directional differences of elastic waves are seen as offering clues to its composition.

The structure was found to be stable at the enormous pressures and to have directionality in the transmission of elastic waves.

Thermal energy in solids is often carried by internal elastic waves, called phonons.

Seismometers are sensors that sense and record the motion of the Earth arising from elastic waves.

Theory of propagation of elastic waves in a fluid saturated porous solid.

Elastodynamics is the study of elastic waves and involves linear elasticity with variation in time.

When they occur in the Earth as the result of an earthquake or other disturbance, elastic waves are usually called seismic waves.

AE is a phenomenon occurring in for instance mechanical loading generating sources of elastic waves.