1. Wind blows waves towards an irregular shoreline with bays and headlands
2. Different parts of the wave will feel the influence of the bottom or seas floor at different stages
3. Directly offshore of headland. The wave will slow down and travel less far
4. But offshore from a bay, the wave will still be in deep water and so travel further
5. As a result, wave and energy is concentrated on both sides of a headland, causing erosion
6. But wave energy is dispersed across a bay, meaning deposition
7. The overall effect is that the wave ends to almost match the shape of the coastline
8. Lastly, because the waves never quite match the shape of the shoreline we still get the process of erosion (hydraulic action)