The East Dundas Tablelands is a large Salinity Province of about 200,000 ha with nearly 5000 ha of mapped dryland salinity occurrence, primarily found along drainage lines, ‘break-of-slope’ and hillside seepage areas, depending upon the Groundwater Flow System (GFS) responsible. The main GFS is deeply weathered and very old volcanic ‘ignimbrite’ bedrock of intermediate scale, with the overlying weathered regolith layers forming local GFSs containing groundwater with salinity ranging from 5000 mg/l to 15,000 mg/l. Groundwater levels undoubtedly increased following landscape clearance but showed a general decline during the drought years. |
Catchment Management Region: | GLENELG-HOPKINS |
Priority Status: | High |
Province Area: | 206,480ha |
Recorded Soil Salinity Area 1: | 4,927 ha |
Dominant Surface Geology Type: | Sedimentary |
Influence of Geological Structure on Salinity Occurrence/s: | None |
Relevant Geomorphological Mapping Units (GMUs): | 2.3.X |
Predominant Groundwater Flow Systems (GFSs): | Local/Intermediate |
Relevant Irrigation Areas: | N/A |