Appendix C - Cultural Heritage Impact Assessment - Peabody Energy
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 />
3.0 Environmental Context<br />
An understanding of environmental context is important for the predictive modelling of Aboriginal sites, as<br />
well as for their interpretation. The local environment provided natural resources for Aboriginal people, such<br />
as stone (for manufacturing stone tools), food and medicines, wood and bark (for implements such as<br />
shields, spears, canoes, bowls, shelters, amongst others), in addition to areas for camping and other<br />
activities. The nature of Aboriginal occupation and resource procurement is related to the local environment<br />
and it therefore needs to be considered as part of the cultural heritage assessment process. The reporting of<br />
environmental context is required under the Code of Practice.<br />
3.1 Geology<br />
Aboriginal people often made stone tools using siliceous, metamorphic or igneous rocks and therefore<br />
understanding the local geology can provide important information regarding resources in a project area.<br />
The nature of stone exploitation by Aboriginal people depends on the characteristics of the source, for<br />
example whether it outcrops on the surface (a primary source), or whether it occurs as gravels (a secondary<br />
source) (Doelman, Torrence et al. 2008).<br />
Most of the project area is characterised by the Late Permian Singleton Supergroup which is part of the<br />
Permian Singleton Coal Measures (sandstone, shale, mudstone, conglomerate and coal seams)<br />
(Department of Mines 1969). The surface geology of the project area is predominantly the Wollombi Coal<br />
Measures in the south-west and Denman Formation of the Wittingham Coal Measures in the north.<br />
Quaternary alluvial silt and sand deposits dominate most of the eastern part of the project area, along the<br />
flats of Wollombi Brook. The Wollombi Coal Measures comprise coal seams in association with<br />
carbonaceous shale, siltstone, sandstone and tuffaceous claystone (Department of Mines 1969). The<br />
Denman Formation of the Wittingham Coal Measures also consists of coal seams and claystone, tuff,<br />
siltstone, sandstone, conglomerate and sandstone siltstone laminate (Sniffin, McIlveen et al. 1988).<br />
Generally, the late Permian Wollombi Coal Measures overlie the Wittingham Coal Measures, which in turn<br />
overlie the mid to early Permian Maitland Group. The Maitland Group in turn overlies the early Permian<br />
Greta Coal Measures which are underlain by the Dalwood Group. These strata layers form the Singleton<br />
Super Group. There is evidence of volcanic activity in the area including felsic volcanics, fault lines and a<br />
number of dykes (Sniffin, McIlveen et al. 1988).<br />
The presence of sandstone in the project area is important for Aboriginal occupation as sandstone was<br />
commonly used for grinding stone artefacts. Overhangs and caves in sandstone cliffs and boulders below<br />
the cliff line were sometimes used for shelter and may be found in the sandstone escarpment to the south<br />
west of the project area. Rock engravings and grinding grooves may be found in areas of exposed<br />
sandstone and sandstone outcrops particularly along creek beds in nearby creek lines such as Wollombi<br />
Brook or North Wambo Creek. Raw materials in the local area including silcrete, indurated mudstone and<br />
silicified tuff, as well as chert, basalt, rhyolite and petrified wood were commonly used by Aboriginal people<br />
for manufacturing flaked stone tools. The softer shales and claystones are highly susceptible to water<br />
erosion processes and are generally unsuitable for the manufacture of stone tools.<br />
3.2 Soils<br />
The predominant soil landscape in the immediate project area is consistent with the Bulga soil landscape,<br />
which consists of smooth slopes forming undulating rises. The Bulga soil landscape is characterised by<br />
sandstone colluviums, yellow and brown solodic soils and brown earths on the lower slopes, with yellow<br />
soloths on the mid slope and upper slopes. Minor to moderate sheet erosion is common (Kovac and Lawrie<br />
1991:125-128). Aboriginal objects may be found in these gently sloping areas.<br />
108453-2; October 2012 Page 14