Hydrogeological Atlas of the Great Artesian Basin. Ransley, T., Radke, B., Feitz, A., Kellett, J., Owens, R., Bell, J. CSIRO Water for a Healthy Country Flagship, Australia. A technical report to the Australian Government from the CSIRO Great Artesian Basin Water Resource Assessment.

Ransley TR and Smerdon BD (eds) (2012) Hydrostratigraphy, hydrogeology and system conceptualisation of the Great Artesian Basin. Volume II: Groundwater Recharge, Hydrodynamics and Hydrochemistry of the Western Great Artesian Basin, National Water Commission, Canberra (eds) 2013, Allocating Water and Maintaining Springs in the Great Artesian Basin. This dataset and associated metadata can be obtained from using catalogue number 81688. The regional flow is inferred to occur down hydrualic gradient perpendicular to groundwater head isopotential contours.

(eds) 2013 (Figure 5.14 Present-day corrected potentiometric surface of the J aquifer for the variable temperature assumption) which was generated from a surface grid that is calculated from temperature and density corrected waterbore head measurements obtained between 20. The composite potentiometric surface contours are modified from (Ransley & Smerdon 2013) (figure 7.4 - Modern (Circa 2010) potentiometric surface) and Love et.al. Ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id= Artesian Basin - Cadna-owie Hooray Potentiometric Surface&rft.identifier= Australia&rft.description=Composite temperature and density corrected potentiometric surface contours for the Cadna-owie-Hooray and equivalents Aquifer and inferred regional groundwater flow directions comprises of two separate data layers Д«: Regional groundwater flow direction arrows - Inferred

Cadnaa user manual