The lateral movement of sand on Fire Island is evident as you look westward from atop the Fire Island Lighthouse, which was built near the end of the island in 1857.
Fire Island is a barrier island, which is believed to have developed as a spit of sediment formed from an eroding headland after the end of the last ice age. Its sand comes from two sources: the eroding cliffs and bluffs of Montauk to its east, and from offshore sources which were deposited by retreating glaciers and remain from earlier inlet deltas.
Fire Island's coastline is constantly being shaped and re-shaped by wind and water. Littoral drift, offshore bottom currents, wind, inlet formation, tidal delta growth, and occasional overwash are all essential to maintain a dynamic equilibrium on a barrier island.