A number of stages were involved in the original headland shape becoming eroded to the present coastal landscape.
Headlands and bays are most likely to be formed in areas where there are alternative bands of soft and hard rock, which meet at right angles to the coast (discordant). The softer rock, for example, clay, will erode more quickly forming bays which make sandy beaches. The harder rock for example, chalk, will erode more slowly forming headlands which jut into the sea. This is called differential erosion.
The erosion occurs due to a number of different processes caused by the sea. Hydraulic action is when the waves smash against the coastline and the force of the water causes the coastline to be eroded.
Abrasion also takes place, this is where the waves pick up rocks and other material and throw it against the coastline, causing further erosion. The coastline can also be eroded due to chemical erosion. Solution is when the acid in the sea water reacts with and erodes the rock such as chalk or limestone.
One of the most common features of a coastline is a cliff. Weathering occurs at the top of the cliff face making it weaker and breaking parts of the rock away. The sea attacks the bottom of the cliff through the processes of hydraulic action, where the water smashes against the rock, abrasion, where the material found in the water wears away the cliff, and solution, where the acids in the water reacts with the rock causing more erosion.
All of the processes come together to form a wave cut notch at the base of the cliff. Over time the wave cut notch is eroded further backwards and when the weight of the cliff above and the force of gravity become too great, the cliff will fall into the sea.
The backwash from the sea carries the material away from the cliff face. The process starts again and repeats itself over time. As the process is repeated the remaining rock as the base of the cliff reduces the force of the waves, this means a wave cut platform is left on the landscape leading up to the new cliff base.