Falaeozic Geology of Victoria. 



SO 



MAP N° 3 



the Macallister, and rises by a long sidling grade more or less 

 parallel with the valley of the creek toi a saddle, thence descending 

 to the Macallister again at Basin Flat by a .similar winding grade 

 cut out of the steep hillside. Tliis part of the road affords a suc- 

 cession of fine soct'ons of the highly inclined Upper Palaeozoic rocks, 



