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Toolinna Cove is the only small pocket of sand on the 160 km long Baxter Cliffs in southeast Western Australia. The cliffs are part of the 790 km long steep southern boundary of the Nullabor Plain located along the western half of Great Australia Bight and facing into the high energy Southern Ocean. The cliffs, which average 90 m in height, are formed from shallow water carbonate deposits and are rich in marine fossils. They consist of a lower (white) Wilson Bluff limestone deposited in shallow seas during the late Eocene and an upper (red) Toolinna and Nullabor limestone deposited during the early Miocene. They were subsequently uplifted to form the level Nullabor limestone plain.

COVER PHOTOGRAPH AND FRONT MATTER: TOOLINNA COVE, BAXTER CLIFFS, WESTERN AUSTRALIA