BY THE REV. J. MILNE CURRAN. 



181 



material, marking the position of ancient river beds, may be 

 studied at Kelso, near the Railway Gates ; near the Church of 

 England grounds ; on the slopes to the right of Kelso-Peel Road, 

 about two miles from Kelso ; on the gravel-topped hills between 

 All Saints' College and the General Cemetery ; near St. Stanislaus 

 College, and generally on the ridges between the Vale Creek and 

 the Macquarie. 



v. Table of formations represented around Bathurst. 



< 



H 



« 



Pn 



Most recent or now in 

 process of forming . . . 



' PostJPliocene 



Volcanic. 

 Pliocene 



Lower Pliocene 



A. Deposits of loam, clay, sand 9 

 gravels and decomposed 

 granites. 



B. Gravels and shingle beds, at 



various levels, between the 

 basalt and the present 

 river bed. 



C. Basalt flow, capping hills. 



D. Clays, sand, gravels, and 

 conglomerates forming 

 " leads " under basalt. 



E. Silicified conglomerates 



older than "leads." 



