The Table Association occurs:
in the Semporna Peninsula to the north of Tawau,
in the Quoin Hill area, and
at Mostyn.
North of Tawau, the association occurs on basalt lava flows, with pronounced terrace features, which are believed to mark the original edges of successive flows. At Mostyn, the lavas occupy an extensive plateau area and basalt boulders form low knolls (mounds). In general, the lava are weathered to depths exceeding 20 ft.