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Appendix C - Cultural Heritage Impact Assessment - Peabody Energy

Appendix C - Cultural Heritage Impact Assessment - Peabody Energy

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<strong>Cultural</strong> <strong>Heritage</strong> <strong>Impact</strong> <strong>Assessment</strong><br />

North Wambo Underground Mine Modification<br />

4.1.3 Campsites and Shelters<br />

J.W. Fawcett (1898:152) described the preferred campsites of the “Wonnah-ruah [sic]” tribal district in the<br />

Hunter River catchment area as being located close to fresh water and food resources. A vantage ground<br />

was also favourable as a precaution against attacks on the camp.<br />

The materials used to construct the campsites and shelters were made from organic matter which is highly<br />

unlikely to have been preserved in the archaeological record.<br />

Fawcett (1898:153) also provided a description of the huts constructed for shelter. These huts were<br />

generally erected using forked sticks planted in the ground with straight sticks laid in the forks and covered<br />

over with sheets of bark sourced from local trees.<br />

4.1.4 Clothing<br />

Summer weather and the milder days of autumn and spring required little in the way of protective clothing;<br />

winter however, saw the use of animal skins for both clothing and as blankets (Heath n.d.:43). Miller<br />

(1886:352) describes Aboriginal people using possum skin cloaks with an ornamental nautilus shell<br />

suspended around the neck on a string.<br />

4.1.5 Burials and Post Contact Phase<br />

There are various reports concerning burial practices of Aboriginal people (Threlkeld in Gunson 1974).<br />

Burials appeared to be the most common form of internment with a well-documented preference for burials in<br />

sandy or loose soils, most likely resulting from the ease of digging a grave (Threlkeld in Gunson 1974).<br />

4.2 Regional Archaeological <strong>Heritage</strong> Context<br />

Archaeological evidence suggests that Aboriginal occupation of the Hunter Valley region began at least<br />

35,000 years ago (Koettig 1987). Additional chronological evidence was recovered from the Hunter Valley’s<br />

northeast mountains for which the following dates were assigned 34,580±650 (Beta-17009), >20,000 (Beta-<br />

20056) and 13,020±360 years before present (BP) (Beta-17271) (Koettig 1987, as cited in Attenbrow 2006).<br />

Kuskie (2000:215) identified artefacts at Wollombi Brook located in a clay horizon that have been dated to<br />

between 18,000 and 30,000 years BP. At Glennies Creek, approximately 50km north-west of the project<br />

area, Koettig and Hughes (1983) excavated a hearth on an alluvial terrace where the radiocarbon-dated<br />

charcoal and geomorphological evidence provided a date of between 10,000 to 13,000 years BP. These<br />

archaeological sites show that the Hunter Valley region was occupied during the Pleistocene, dated up to<br />

11,000 years ago (Short 2000); Pleistocene sites are generally rare and therefore contain significant<br />

archaeological/scientific information as well as demonstrating the long occupation of Aboriginal people in the<br />

region.<br />

The majority of Aboriginal sites in the region, however, are dated to the more recent Holocene (

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