80 
paringa, a clay in all respects similar to the glacial clays of 
southern Yorke's Peninsula, rises from beneath the fossili- 
tation has hitherto bien felt in testing the beds to the 
lacial h i 
that they belong to the same aa 
no reason dá conclude that the extent of the 
glacial area in South Australia has even yet been fully - 
determine he limits of the evidence on Yorke’s Penin- 
e 
further to the west. It is Hii directions that further 
investigations should be adult 5 ; 
acknowledgments are due to Mr. E. H. Matthews, of 
^ a; 
well, junr., Honit ; and Mr. William Fowler, Yararoo, for 
information and aem facilities by which I was enabled to 
utilise the short time at my disposal to the best advantage. 
