The layered sandstones and siltstones (mudstones) are seen in the cliff faces and also form the shore platform around the north and west sides of the park.
The shore platforms are therefore clearly polycyclic and contain inherent morphological features but are being actively rejuvenated by the removal of cover deposits.
It also displays coastal geomorphology which demonstrates a particularly well-developed series of intertidal shore platforms varying in width from about 200-600m.