Henperson.—Post-Tertiary History of New Zealand. 599 
101. Apxry, б. L., 1919. Horowhenua Coastal Plain. Vol. 51. 
102. —— . Tararua Drainage. Vol. 52. 
103. Morean, P. G., 1921. Patea District. Vol. 53. 
104. Соттом, C. A., 1921. Warped Land-surface, Port Nicholson. bid. 
2 2 d. Ibid. 
921. Porirua Harbour. Ibid 
106. Арктх, G Б bid. 
1921. Waikato Heads District. bid. 
Re) mene | 
107. GILBERT, M. J., 
Miscellaneous Publications. 
108. vox Haast, J., 1861. Report of a Topographical and Geological Exploration of 
the Western Districts of the Nelson Province, New Zealand. 
109. Hector, J., 1863. Geological Expedition to the West Coast of Otago, New Zea- 
land, Otago Provincial Gazette, vol. 6. 
110. vox Haast, J., 1864. Report on the Formation of the Canterbury Plains. 
111. уох Hocusterrer, F., 1867. New Zealand. 
112. Ноттох, Е. W., and Urnicn, G. Н. F., 1875. Report on the Geology and Goldfields 
tago. 
113. vox Haast, J., 1879. Geology of the Provinces of Canterbury and Westland, New 
nd. 
114. cpa ide x W., 1885. Sketch of the Geology of New Zealand, Quart. Jour. Geol. 
., vol. 41. 
115. MansHaLL, P., 1906. The Geology of Dunedin, New Zealand, Quart. Jour. Geol. 
Soc., vol. 62. 
116. Park, J., 1910. The Geology of New Zealand. 
117. Tuomrson, J. B., 1910. Drainage Operations in Hauraki Plains. C.-8 (Parlia- 
mentary Paper). 
118. MARSHALL, P., 1912. New Zealand andAdjacent Islands. 
119. —— 1912. Geo of New Zealand. 
Evidences of Pleistocene Glaciation at Abbotsford, near Dunedin. 
By Professor James PARK, Е.С.8., F.N.Z.Inst., Dean of the Faculty of 
7 + 
Mining at Otago University. 
[Read before the Otago Institute, 13th November, 1993 ; received by Editor, 3rd December, 
1923; issued separately, 28th August, 1924.) 
local 
deposit as a boulder-clay. Had the beds a glacial origin boulders of schist 
would naturally occur, since that rock outcrops at no great distance from 
the clay.” 
The aforesaid boulder-clay formation occupies the floor and slopes of 
the Abbotsford basin. From about 100 ft. above the sea it rises gently 
northward to a height of 475 ft. Generally it ranges from a few feet to 
* Trans. N.Z. Inst., vol. 53, pp. 157-74. 
+ The Great Ice Age of New Zealand, Trans. N.Z. Inst., vol. 42, pp. 580-612. 
