Estate & Source

Water is shaped by place.

Carribie Estate lies beneath coastal dune systems on the southern edge of South Australia’s Yorke Peninsula, overlooking the Great Southern Ocean.

Remote. Geologically stable. A landscape defined by wind, sea and time. Such conditions are increasingly rare globally and rarely protected.

At Carribie, winter rains fall onto a landscape of ancient aeolian calcarenite—coastal dune systems formed by wind over millennia, their fine marine sands bound into soft limestone. Through layers of calcareous sands, shell fragments and dense limestone laid down 540 million years ago, water moves slowly.

Beneath lies the Carribie Basin aquifer, where water rests, evolves and finds balance.

Formally documented in a 1966 South Australian Government hydrogeological study, identifying the aquifer as a naturally recharging freshwater limestone aquifer of “excellent quality.” A rare instance of early scientific validation of a mineral water source.

NOTHING IS ADDED. NOTHING IS ADJUSTED. CARRIBIE IS FORMED OVER TIME.