Aboriginal History Radio-carbon dating of cultural material has established that Aborigines were resident as long ago as 5,500 years BP (before present). It is possible that evidence of earlier occupation may still lay entombed in the sands of the Great Sandy Region. Age determination by radio carbon dating placed the time of formation of the Continue reading
Aesthetics
Great Sandy Soils
Fraser Island and the adjoining Cooloola sandmass (covering a total of approximately 200,000 hectares) consist almost entirely of quartz sands that have accumulated during episodic periods of dune building in the Quaternary. At least eight dune systems have been identified at Cooloola and nine systems at Fraser Island marking separate episodes of deposition above sea Continue reading
Marine areas of Hervey Bay and Great Sandy Strait
Most of the marine areas of Tin Can Bay, Great Sandy Strait and Hervey Bay formed behind the large coastal dune fields of Fraser Island and Cooloola sand masses when the sea level rose to its present level about 7000 years ago. The waters of Great Sandy Region are protected from southerlies through to easterlies Continue reading
Quotes Describing Fraser Island
From Historical Documents and Literature From its earliest days FIDO has sought to collect any written records which might give a clue to what constitutes Fraser Island’s integrity. FIDO has also tried to gather in as many old photographs as possible to provide a visual guide to integrity. As far as possible FIDO has sought Continue reading
Wilderness Values of Fraser Island
What is Wilderness? Wilderness has almost as many dimensions as the number of people who consider it. However, there is some consensus about the main elements of wilderness. It has three essential attributes – naturalness, remoteness and size. A wilderness area is defined as having, or as being capable of restoration to: a sufficient size Continue reading