All forms of waves carry energy; this is directly visualized in nature. For instance, the waves of earthquakes are so intense that they can shake huge concrete buildings, causing them to fall. Loud sounds can damage nerve cells in the inner ear, causing permanent hearing loss. The waves of the oceans can erode beaches.
In mechanical waves, the amount of energy is related to their amplitude and frequency. In the context of the above examples, large-amplitude earthquakes produce large ground displacements. Loud sounds have high-pressure amplitudes and come from larger amplitude source vibrations than quiet sounds. Large ocean waves can agitate the shore more than small ones.
The energy carried by a wave has two major components: kinetic energy and potential energy. Consider a seagull floating on the waves of the sea. The waves do the work of moving the seagull up and down. The larger the wave's amplitude, the higher the seagull is lifted, therefore the more significant the change in potential energy. Remember that the energy of the wave depends on frequency too; if the energy of each wavelength is assumed to be a discrete packet of energy, a high-frequency wave will deliver more of these packets per unit of time than a low-frequency wave.
This text is adapted from Openstax, University Physics Volume 1, Section 16.4: Energy and Power of a Wave.
