BY R. M. JOHNSTON, F.LS. 133. 
(10) 1886—Fresh evidence of huge ice-borne erratics em- 
bedded in rocks of Permo-Carboniferous age at 
One Tree Point, Bruni Island. R. M. 
Johnston. Proc. Roy. Soc. Tas., 1886, pp. 23, 24.. 
(11) 1887—Glacial phenomena in South Australia. Prof, 
Ralph Tate, F.G.S. F.L.8. Proc. Aus. Ass. for 
Adv. of Science, Sydney, 1887, pp. 231, 232. 
(12) 1888—Observations regarding recent glacial phenomena 
in the western highlands of Tasmania. John- 
ston, Geol. of Tasmania, p. 164. Ibid, pp. 
215, 216. 
(18) 1888—Climate of the Neogene period in Tasmania, with 
observations bearing upon the evidence of gla- 
ciation in the higher levels of the western high- 
lands, and discussing the views of Croll, Wal- 
lace, Hutton, and others, respecting the 
necessary conditions for the production of a 
true glacial epoch equivalent to that of the 
pleistocene period of Hurope and North America. 
R. M. Johnston. Geol. of Tasmania, pp. 
254-257. 
(14) 1888—Lack of evidence of a severe glacial period in 
the pleistocene rocks of Australia and Tas- 
maniaascribed to the absence of such geographical 
conditions as would bar the intrusion of warm 
equatorial currents at the last period of maxi- 
mum eccentricity combined with winter in 
aphelion. R.M. Johnston. Geol. of Tasmania, 
pp. 296, 297. 
(15) 1890—Review of evidence relating to ice action at close 
of Permo-Carboniferous rocks in Victoria, New 
South Wales, Queensland, South Africa, and 
India. Dr. Feistmantel—Memoir of Geo. Sur. 
of N. 8S. Wales—Pal. No. 3, pp. 174-183. 
(16) 1890—Further confirmation of Daintree’s and Selwyn’s 
views respecting the glacial character of the 
Bacchus Marsh conglomerates (Permo-Car- 
boniferous), Victoria. E, J. Dunn. The 
Glacial Conglomerates of Victoria. Proc. 
Austral. Assoc. for Ady. of Science, pp, 452- 
458, 1890. 
