3. Southern Uplands (SU)
3.1.1 Plateaux and broad ridges (Beech Forest, Wyelangata, Balook)
3.1.2 Ranges (Forrest, Barramunga, Poowong, Fish Creek)
3.1.3 Basalt residuals (Thorpdale, Nerrim South)
3.1.4 Prominent hills (Wilsons Promontory)
|These comprise the Otway, Strzelecki and Hoddle Ranges and Wilsons Promontory. The Otway, Strzelecki, and Hoddle Ranges have all been a result of significant uplift occurring in the recent geological past along north-easterly trending fault lines. In the Otway Ranges, this has occurred along two reverse faults: the westerly dipping Torquay fault to the east and the Bambra fault to the west (Joyce, Webb et al. in press) with an estimated 175 to 240 m of uplift occurring in the Late Neogene (Sandiford 2003).|
The Strzelecki and Hoddle Ranges have also resulted from a series of north-easterly trending fault lines and monoclines. Some examples are the Bass fault near Loch, the Yarragon monocline south of Yarragon, the Kongwak fault north of the Powlett River, the Budgeree fault south of Churchill and the Yarram monocline west of Yarram. These faults have resulted in a major alteration of the Late Paleogene to Early Neogene stream pattern as evidenced by the presence of their sediments on both the northern and southern flanks.