Coastal sites in northern NSW date to within the Holocene period. The earliest of these is a shell midden at the base of East Banora Point on the lower Tweed River where an occupation phase was dated between 4,700 BP and 4,200 BP (Appleton 1993:34). Faunal material showed a predominance of oyster, cockle and whelkContinue reading “Rocks and Headland Hastings Point”
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