Abstract

The Australian State of Tasmania, at latitude 42 degrees south, became an island about 8,000 years ago when the sea rose to its present level, following the melting of polar and glacial ice that covered much of the land mass. After that time, the Tasmanian Aboriginal rock art developed independently of mainland Australia, with its form being basically linear with some naturalistic figures and a predominance of cupules. The petroglyphs with one lithophone site occur on various rock substrates varying in hardness from granite to sandstone. Many sites exist along the western coastline that borders the Southern Ocean where the landscape in some places has changed little since the arrival of Europeans in 1803. The significance of this Tasmanian Aboriginal cultural heritage along what is now known as the Tarkine Coast, named after an Aboriginal band that once inhabited this area, was recognised by the Australian Government in February 2013 when a 21,000 ha strip, 2 km wide, was inscribed on its National Heritage Register, being one of 98 special places listed in the country. However, politics and racism hamper its management. This paper is based on the results of 40 years of field recording of the Tasmanian Aboriginal rock art sites, many of which remain unpublished.

Highlights

  • The Australian State of Tasmania, at latitude 42 degrees south, became an island about 8,000 years ago when the sea rose to its present level, following the melting of polar and glacial ice that covered much of the land mass

  • The significance of this Tasmanian Aboriginal cultural heritage along what is known as the Tarkine Coast, named after an Aboriginal band that once inhabited this area, was recognised by the Australian Government in February 2013 when a

  • As people moved south into Tasmania, the traditional expressions of rock art followed, and were maintained after they were isolated when their land was separated by the rising sea levels

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Summary

Climate and Early Migration South

Tasmanian human occupation dates back more than 40,000 years to when sea levels were much lower than at present, during the last Ice Age which exposed the land linking south-eastern. In 1974, an archaeologist Sandra Bowdler found Aboriginal occupational material evidence that dated back 23,000 years during an excavation of a cave on what is Hunters Island, about 6 km off the north-west corner of Tasmania. From the evidence she unearthed, it was determined that food came not from the sea, as the nearest coast would have been 75 km away to the west, but from plants and animals of the inland plains.

Tasmanian Highland Petroglyphs
The Significance of Tasmanian Xenoliths
Petroglyphs of the West Coast
The Status of Petroglyph Sites and Threats
Findings
Conclusion
Full Text
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