Began during the last ice age (14,000). Originated from the rivers from the Southern Alps. The sediment mostly consists of granite and schist which forms the bedrock in the area, and is carried by the Tasman sea. The sediment is northwards by the Westland current. There’s an abrupt change in the coasts direction due to Golden Bay and sediment continues into Greater Cook Strait as LSD is stronger. As the spit increases in length, the tidal currents increase in speed, and so the sediment load and erosion rate increase.