Cenozoic northward drift of the Australian plate was determined from paleomagnetism of Middle Eocene through Pleistocene sediment cores from ODP Leg 182 (Sites 1126, 1128, and 1134) in the Great Australian Bight. Paleolatitude estimates are based on stepwise AF and thermal demagnetization of approximately 400 discrete samples, of which approximately 250 provided reliable data. The characteristic magnetization of the sediments resides in magnetite and magnetic sulfides. Middle Eocene through Lower Oligocene ( approximately 36 Ma) paleolatitudes of approximately 52 degrees (+ or -2 degrees ?) change gradually to Late Miocene ( approximately 9 Ma) paleolatitudes of approximately 48 degrees (+ or -2 degrees ). These data, combined with Australian paleomagnetic pole data, indicate a slow rate of northward motion through much of the Cenozoic ( approximately 28 mm/yr). These data also indicate an abrupt acceleration in the Late Miocene (drift rate approximately 115 mm/yr), coinciding with tectonic events in Southeast Asia. Paleolatitude estimates support Miocene versions of the Australian apparent polar wander path that place the Oligocene-Miocene pole ( approximately 25 Ma) at approximately 70 degrees S-125 degrees E and the Late Miocene pole at approximately 70 degrees S-105 degrees E (e.g., Idnurm, 1985, 1994). Inclination data for discrete samples also provide a refined magnetostratigraphy for portions of the Miocene, Oligocene, and Eocene carbonate and siliciclastic section of the Great Australian Bight.