Key finding 2:
The West Casino Gas Project is hydrologically disconnected from the Jeebropilly Mine by a geological basement ridge that forms a natural barrier separating the and in the Richmond river basin in NSW from those of the Bremer river basin in Queensland.
Key finding 3:
Groundwater flow from the Lamington and Main Range volcanics to near-surface (alluvial) aquifers and associated streams is much greater than any potential drawdown due to additional coal resource development, minimising potential impacts.
To enable accurate hydrological modelling of areas of potential change, a bioregion-wide three-dimensional geological model was developed for the assessment (Figure 2). The model provided an understanding of the bioregion’s geology and to identify pathways between different parts of the hydrological cycle.
Analysis of the model demonstrated that a geological ridge forms a natural barrier separating the Richmond river basin in NSW and the Bremer river basin in Queensland. This means the West Casino Gas Project is hydrologically disconnected from the Jeebropilly Mine. Because of this, and because the assessment focused on potential impacts due to (Box 2), only the West Casino Gas Project was modelled.
The analysis based on the geological model also improved understanding of the geological structure and layers, helping to map the three-dimensional extent of the Walloon Coal Measures, the main target of CSG exploration in this bioregion, and other key aquifers such as the alluvium and Lamington Volcanics, as well as including the MacLean Sandstone, Bungawalbin Member and parts of the Grafton Formation (Figure 3). In addition, it highlighted the role of the outcropping Lamington Volcanics in NSW and Main Range Volcanics in Queensland as the main areas in the bioregion. These aquifers are mostly less than 200 m thick but are locally up to 900 m thick near major extinct volcanoes. Due to its regional extent, considerable thickness and high rates, the Lamington Volcanics form a major regional aquifer system with a very large storage volume, which sustains permanent or near-permanent flows in most major streams within the Richmond river basin.
The groundwater recharge assessment showed that within the Richmond river basin, groundwater recharge rates to the Lamington and Main Range volcanics are at least ten times higher than recharge rates to sedimentary bedrock units such as the Walloon Coal Measures. A large proportion of groundwater recharge to the Lamington Volcanics discharges locally with short transit times into the alluvium or streams, with only a small proportion percolating to deeper aquifers. This means that water in alluvia or streams associated with the Lamington Volcanics is generally fresh, whereas in the sedimentary bedrock is typically brackish or saline.
Conceptual about the between deep and shallow aquifers in general, and the role of faults as potential pathways linking the Walloon Coal Measures to shallow aquifers and features in the Richmond river basin, are further explained in ‘How to use this assessment’.
Figure 2 Three-dimensional geological model of the Clarence-Moreton bioregion viewed from the south-east, showing the distribution of the different types of aquifers (alluvial, volcanic and sedimentary bedrock)
The vertical extent is from –2500 to +1400 m Australian Height Datum (AHD). The north–south extent is 320 km; the maximum east–west extent is 140 km; and the vertical exaggeration is 10. Vertical exaggeration is the scale used in raised-relief maps to emphasise vertical features that might be too small to identify relative to the horizontal scale.
This cross-section is a stylised representation from the geological model, and has been vertically exaggerated (by a factor of 12, both above and below ground) in order to make it easier to distinguish the relationship between different geological units. The additional coal resource development (ACRD) only includes the West Casino Gas Project.
mAHD = metres above Australian Height Datum
Product Finalisation date
- Explore this assessment
- About the bioregion
- How does the bioregion's geology and hydrogeology influence water movement?
- How could coal resource development result in hydrological changes?
- What are the potential hydrological changes?
- What are the potential impacts of the hydrological changes?
- How to use this assessment
- Building on this assessment
- References and further reading
- Contributors to the Technical Programme