attempt is made to correlate stratigraphically these upland 

 Eocenes with their low-level equivalents. 



The observations detailed in this paper, whilst enlarging our 

 knowledge of the geographical extent of the extinct ice-field of 

 South Australia, unfortunately, do not throw any additional 

 light on the age at which the glaciation took place or the kind of 

 agency by which the ice operated. We may reasonably expect, 

 however, that when the thick and varied deposits of this period 

 have been submitted to careful examination these two questions 

 will be solved. 



