315 



Tate, R., and J. Dennant. 



1896 — "Correlation of the Marine Tertiaries in Australia, part III., South 

 Australia and Tasmania," Trans. Roy. Soc. S. Austr., vol. xx., 

 p. 118, pi. ii. (See correction of plate in "Erratum," on slip, 

 vol. xxi., fronting "Contents.") 



Tate, Howchin, and David. 



1895 — "Glaciation at Hallett's Cove" (Glacial Research Com.), Aus. Assoc. 

 Adv. Sc, vol.'vi., p. 315, pis. xlix. and 1. 



Woods, J. E. Tenison. 



1878 — "Some Fossil Corals from Aldinga," Phil. Soc. of Ad. (Roy. Soc. 

 S. Austr.), vol. i., p. 104, pis. i. and ii. 



DESCRIPTION OF PLATES XXII. to XXVI. 



Plate XXII. 



Fig. 1. View of the southern face of Blanche Point. The foreground shows the beach 

 platform consisting of the fossiliferous Miocene. The same beds form the lower portion of 

 the cliff up to three-fourths of its height. The upper part of the cliff is formed by the Lower 

 Pliocene fossiliferous sands overlain by a white hmestone. The base of the newer fluviatile 

 beds is seen resting on the latter at the right-hand side of the picture. 



Fig. 2. View taken from the top of Blanche Point Cliff, looking southwards, at the same 

 level. The white-coloured Lower Pliocene limestone forms a platform and a white ridge, 

 seen on the right-hand of the picture. On this platform the Pleistocene and Recent alluvia 

 form a secondary cliff which is undergoing sculpture and waste by atmospheric weathering. 



Plate XXIII. 



Fig. 1. Photograph of a raised beach of large stones now included within the area of 

 the sandhills on the northern side of Pedler's Creek. 



Fig. 2. An outlier (or butte) of the alluvial cliffs on the northern side of the outlet of 

 Morphett Vale Creek. The main portion of the hill is composed of Pleistocene clays and 

 indurated sands ; a strong bed of sandstone forms the crest of the hill, and the white sand bed, 

 underlying the Lower Pliocene bed, can be seen near the base of the hill, although somewhat 

 obscured by talus. The hill is strikingly similar in outline to Crown Point Hill, on the Finke 

 River, but is not so high. 



Plate XXIV. 



Fig. 1. A view of the thick gravel beds that form the main cliff for about a mile in 

 length on the coast, near Sellick's Hill, and are about 200 feet in height. 



Fig. 2. Another view of the same gravel beds at a short distance from those shown 

 in fig. 1. 



Plate XXV. 



_ ■ Geological section of the sea-cliffs from Brighton (bore) to the mouth of the Onkaparinga 

 River. 



Plate XXVI. 

 Geological section of the sea-cliffs from the mouth of the Onkaparinga River to the 

 beach near Sellick's Hill. 



