AUSTRALIAN GLACIATIONS 222 
this part of Tasmania to the height of several hundred feet, so that some of 
the glaciers may have actually reached sea level (XXXIX, p. 52). 
More extended observations will probably show that in both 
Australia and Tasmania this latest of Australian glaciations was 
much more extensive than at present known. 
In considering the climatic and physiographical conditions of 
Australasia in the Pleistocene period, it is important to take into 
account the greater development of glaciers in New Zealand at 
about that time (XL, XLI). 
BIBLIOGRAPHICAL REFERENCES (SELECTED) 
CAMBRIAN GLACIATION 
SOUTH AUSTRALIA 
(1) tgo1. Howchin, W. ‘Preliminary Note on the Existence of 
Glacial Beds of Cambrian Age in South Australia.” 
Trans. and Proc. Roy. Soc. S. Aus., XXV, 10-13. 
(II) 1900. “The Geology of the Mount Lofty Ranges,”’ 
Part, Trans. and Proc. Roy. Soc. S. Aus., XXX, 228-34, 
pl. XII. 
(IIT) 1908. “Glacial Beds of Cambrian Age in South 
Australia,’”’ Quar. Jour. Geol. Soc., LXIV, 234-59, figs. 1- 
TAR Gs 20D, O.QV f. 
PERMO-CARBONIFEROUS GLACIATION 
SOUTH AUSTRALIA 
(IV) 1887. TaTE, R: “Glacial Phenomena in South Australia 
(Hallett’s Cove),” Rep. Aus. Assoc. Adv. Science, I, 
231-32, sydney. 
(V) 1895. TATE, Howcuin, and Davin. “Evidences of Glacia- 
tion at Hallett’s Cove,” Rep. Aus. Assoc. Adv. Science 
(Report of Glacial Research Committee), VI, 315-20, 
pis DXA. 
(VI) 1808. ‘‘Report of Glacial Research Committee, South Aus. 
Evidences of Glaciation in the Inman Valley, Yankalilla, 
and Cape Jervis Districts,” Rep. Aus. Assoc. Adv. 
Science, VII, 114-27, pls. I, III, and fig. in text (photo- 
graphs of striated pavement and large erratic). 
(VII) 1898. Howcnin, W. ‘Further Discoveries of Glacial Remains 
in South Australia (Hindmarsh Valley),” Trans. and 
PrOG. ROY. SOC. S-AUS., SONI 12=17- 
