The pebbles that are to be found on a beach are invariably round and smooth owing to the constant battering they have received from the sea. Originally pebbles were part of much larger rocks, but various natural phenomena, such as earthquakes and volcanoes, have gradually broken them down.
When caught in the movement of sea, and constantly rubbed against other hard materials, the pebbles finally lose their irregularities and present a smooth round surface. Many of the rocks of today will be pebbles in thousands of years’ time, and many of today’s pebbles will eventually be turned into sand by the constant, wearing action of the sea.
A beach composed chiefly of surface pebbles is commonly termed a shingle beach. This type of beach has armoring characteristics with respect to wave erosion, as well as ecological niches that provide habitat for animals and plants. Inshore banks of shingle (large quantities of pebbles) exist in some locations, such as the entrance to the River Ore, where the moving banks of shingle give notable navigational challenges.

