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Andersons Bay was formed aѕ "the result of the land sinking below 1000 feet and the sea entering two river valleys to form the harbour as we now know it. Later rivers such as the Taieri and the Clutha deposited eroded materials in the sea with the prevailing currents carried north-easterly to deposit and create the narrow isthmus between the sea and the harbour, forming an extensive mud-flat. Former inlets of the sea became land-locked to leave traces of their origin - a former island, Sunshine and part of Musselburgh, and the cliffs of Tainui and Bayfield .By the time of European settlement the Andersons Bay district was described as being of bush-clad hills, flax-covered swamps and an indented low-lying harbour and coastal shoreline.

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