GLACIAL BEDS, LITTLE PEPPERMINT BAY. 47 



quite, at the base of the Permo-Carboniferons series. The 

 Little Peppermint Bay beds lie almost certainly on a much 

 hiiD'her horizon. Further examination may tend to show 

 that in S.E. Tasmania the glacial beds are related to each 

 other in a manner somewhat similar to that of the glacial 

 beds at Lockinvar and Branxton, New South Wales, as 

 described by Professor David, F.R.S. (Proc. Roy. Soc, 

 IS .S.Wales, 1899, p. 154). 



