Salinity is likely to expand with moderate consequences, although timing of salinity may be extended because of changes in rainfall pattern. Southern 2 26 mostly falling possible insignificant long term low Groundwater levels within the Cross (9) greenstone ranges are deep Falling groundwater trends occur in all lower-catchment bores, with variable trends in mid and upper catchment bores. Depending on climate, the time to a post-clearing hydrological equilibrium may be decades away. The salinity risk is low because salinity could possibly occur in the future but with insignificant consequences. 6 26 variable likely moderate medium moderate A large number of bores in the Zone term hydrozone now have stable of Ancient groundwater trends. However, Drainage (10) rising trends still occur in upland areas and in areas of A H A V F hazard in the south of the hydrozone where rainfall is highest. Salinity is likely to continue to develop, albeit at a reduced rate because of reduced rainfall. Future salinity
Salinity is likely to expand with moderate consequences, although timing of salinity may be extended because of changes in rainfall pattern. Southern Cross (9) 2 26 mostly falling possible insignificant long term low Groundwater levels within the greenstone ranges are deep Falling groundwater trends occur in all lower-catchment bores, with variable trends in mid and upper catchment bores. Depending on climate, the time to a post-clearing hydrological equilibrium may be decades away. The salinity risk is low because salinity could possibly occur in the future but with insignificant consequences. Zone of Ancient Drainage (10) 6 26 variable likely moderate medium term moderate A large number of bores in the hydrozone now have stable groundwater trends. However, rising trends still occur in upland areas and in areas of A H A V F hazard in the south of the hydrozone where rainfall is highest. Salinity is likely to continue to develop, albeit at a reduced rate because of reduced rainfall. Future salinity