1. Firstly, the sea attacks the foot of the cliff and begins to erode areas of weakness such as joints and cracks, through processes of erosion such as hydraulic action and abrasion.
2. Gradually, the cracks get larger, developing into small caves. Further erosion, widens the cave and where the fault lines run through the headland, two caves will eventually erode into the back of each other forming an arch, passing right through the headland.
3. The combination of wave attack at the base of the arch, and weathering of the roof of the arch (frost, wind and rain) weakens the structure until eventually the roof the arch collapses inwards leaving a stack, a column of rock which stands separate from the rest of the headland.
4. The stack continues to erode, eventually collapsing to form a stump which may be covered by water at high tide.