RELATIONSHIPS OF THE AUSTRALIAN CAINOZOIC SYSTEM. 
from this point to the junction bears the aspect of a rejuvenated 
stream, flowing in a deep, entrenched valley ( see Fig. 16). The 
line of fault referred to passes almost due north and south 
Fig it. op the Qrkn<;e Burr betweer h enty’s an d the 
Junction) with t^uDOY CREEK 
cutting the Muddv Creek at MacDonald’s, 1 mile south of 
Forsyth’s (see sketch map big. 13). The effect of this fault is 
seen on the course of the Grange Burn below Forsyth’s, where 
the mature stream, after coming from Hamilton and flowing 
over Kalimnan strata (Fig. 17), taking a more northerly turn, cuts 
through high banks of polyzoal limestone resting on quartz porphyry, 
thence flows to the west for 20 chains, and then southward for another 
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° ' Forsyth's. 
20 chains, after which it follows its normal westerly course towards 
the Wannon. On the same area of uplift at Muddy Creek, starting 
from Clifton Bank, the Balcombian beds gently dip, with some 
slight undulations, towards MacDonald’s, but are still seen at a 
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