Falaeozic Geology of Victoria. 



SO 





C-^v «„\-> »-....-.jt.M ""v W '^/V/ -■'•'*■■'- ■ J 







. --. .... '• ... .K; . ri . 











MAP N°3 ■'™"™™"™"°" 



the Macallister, and rises by a long sidlinii: grade more or lees 

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

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

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

 cession of fine scct'ons of the highly inclined Upper Palaeozoic roi-ks,. 



