In plan view, the outline of the coast often shows headlands and geos. The geos can usually be traced to lines of weakness provided by trap dykes, faults and master joints. The headlands, as well as showing relatively low fracture densities, often relate to resistant rocks
The detailed cross-sectional form of cliffs is a product of rock structure. Many cliffs drop into deep water and this precludes effective abrasion of the cliff base. The cliff face may be tens or even hundreds of metres high but can be divided into a number of zones according to the influence of waves and spray. At the base is the submerged zone, hidden from view. Close to sea level lies a zone of inundation which is exposed to the air only between waves. Above this lies a wave impact zone, which is pounded by waves under higher sea states. The highest marine influence is in the spray and wash zone, where water from breaking waves shoots upwards as droplets or sheets. All four zones vary in height according to the sea state. Only during conditions of low tide and low swell can the inundation zone be observed easily and at these times wave and spray action will be confined to the lowest parts of the cliff. Under high sea states, where deep water waves up to 15 m high can approach the shore, wave action reaches heights of 25 m on some cliffs, wash strips vegetation and loose debris and spray and air borne debris is carried many tens of metres inland. Rock fragments and granules thrown by the wind may create a depositional zone on cliff tops, a form of machair in which progressive soil thickening incorporates clasts from cobble size downwards.