Companion product 1.1 for the Galilee subregion () provided some background information on surface water systems in the , with companion product 1.5 () providing further detail on usage and water quality.
Major river basins and associated drainage are outlined in Figure 18. The Galilee subregion straddles the Great Dividing Range and includes the headwaters of six major river basins. These are the eastward draining Burdekin and Fitzroy river basins; the Cooper Creek – Bulloo and Diamantina river basins, which drain westwards; the northward draining Flinders-Norman river basin; and the Warrego river basin, which drains southwards.
Much of the Galilee subregion lies in the Cooper Creek – Bulloo and Diamantina river basins (Figure 18). However, most of the proposed coal mine developments are located in the Burdekin river basin. The most advanced coal mine developments are situated on the western side of the Belyando river basin. Proposed CSG projects occur in the Cooper Creek – Bulloo river basin. However, these projects are at a less advanced stage (see Section 2.3.4 and companion submethodology M04 (as listed in Table 1) for developing a coal resource development pathway ()). As of December 2016, there are no commercially producing coal resource developments in the Galilee subregion.
Streamflow in the Cooper Creek – Bulloo and Diamantina river basins are strongly seasonal and, from year to year, flows can vary greatly from almost no flow to significant floods. Streamflow in the portions of the Burdekin, Fitzroy and Flinders-Norman river basins that lie within the Galilee subregion are characterised as dry seasonal flows. Although flows vary greatly between months with minimal to no flow from July to October, most flows occur between December and April. The flow regime for Warrego river basin, while highly variable, is classed as perennial (companion product 1.1 for the Galilee subregion ()). Much of the river flow in the Warrego river basin occurs between December and April.
There are some closed drainage basins that are associated with significant lakes such as Lake Galilee and Lake Buchanan and they occur between the Great Dividing Range, and the ranges that demarcate the eastern edge of the Eromanga Basin (Figure 18). These lake basins are largely confined on their western side by series of hills that define a long arcuate ridge that runs parallel to the Great Dividing Range. These hills mostly comprise outcropping Eromanga Basin rocks, in particular, the Hutton Sandstone and Ronlow beds.
Product Finalisation date
- 2.3.1 Methods
- 2.3.2 Summary of key system components, processes and interactions
- 2.3.3 Ecosystems
- 2.3.4 Baseline and coal resource development pathway
- 2.3.5 Conceptual model of causal pathways
- Currency of scientific results
- Contributors to the Technical Programme
- About this technical product