CSIRO Publishing The Royal Society of Victoria, 130, 14–31, 2018 www.publish.csiro.au/journals/rs 10.1071/RS18004 THE MOYJIL SITE, SOUTH-WEST VICTORIA, AUSTRALIA: STRATIGRAPHIC AND GEOMORPHIC CONTEXT STEPHEN P. CAREY1, JOHN E. SHERWOOD2, MEGAN KAY1, IAN J. MCNIVEN3 AND JAMES M. BOWLER4 1School of Science, Engineering and Information Technology, Federation University Australia, PO Box 663, Ballarat, Victoria 3353, Australia 2School of Life and Environmental Sciences, Deakin University, PO Box 423, Warrnambool, Victoria 3280, Australia 3ARC Centre of Excellence for Australian Biodiversity and Heritage, Monash Indigenous Studies Centre, Monash University, Melbourne, Victoria 3800, Australia 4School of Earth Sciences, The University of Melbourne, Victoria 3010, Australia Correspondence: Stephen Carey,
[email protected] ABSTRACT: Shelly deposits at Moyjil (Point Ritchie, Warrnambool), Victoria, together with ages determined from a variety of techniques, have long excited interest in the possibility of a preserved early human influence in far south-eastern Australia. This paper presents a detailed analysis of the stratigraphy of the host Bridgewater Formation (Pleistocene) at Moyjil and provides the context to the shelly deposits, evidence of fire and geochronological sampling. We have identified five superposed calcarenite–palaeosol units in the Bridgewater Formation, together with two prominent erosional surfaces that may have hosted intensive human activity. Part of the sequence is overlain by the Tower Hill Tuff, previously dated as 35 ka. Coastal marine erosion during the Last Interglacial highstand created a horizontal surface on which deposits of stones and shells subsequently accumulated. Parts of the erosional surface and some of the stones are blackened, perhaps by fire.