52 T. S. Hall: 



we approach the phiteau near Anglesea from the hiva-tioored 

 valley, the heights are rather striking, and are dignified by 

 the name of the Anglesea Ranges. Once on the plateau the 

 eoast road easily avoids all valleys, and runs level till the 

 Anglesea Valley is reached. This near its mouth is about three 

 miles wide, and is trenched to a depth of about 200 feet. To- 

 wards Airey's Inlet the elevation increases as the beds begin 

 to rise on the flanks of the Jurassic, and the streams have 

 greater cutting power, and are more numerous, so that broad 

 stretches of level country are less frequent. 



Airey's Inlet is curiously named, for there is no inlet from 

 the sea ; the small creek is usually barred completely by sand 

 banks, but was possibly opened by floods at the time it was 

 named. 



The valley of Spring Creek is a modern one, and is steep- 

 sided near the township of Jan Juc, where a faii'ly fertile soil 

 is derived from the waste of the earthly limestones exposed. 



I give a list of the fossils I have identified frou) my gather- 

 ings at Point Addis and Airey's Inlet (Split Point), and quote 

 their Spring Creek record: — 



Airey's. Addis. ^^ 



Paradoxechinus novus, Laube 1 1 1 



Monostychia australis, Laube 1 1 1 



Scutellina patella, Tate 1 1 1 



Fibularia gregata, Tate 1 — 1 



Cassidulus australiae, (Duncan) 1 1 1 



Eupatagus murrayensis, Duncan 1 1 1 



Eupatagus rotundus, Duncan — 1 I 



Duncaniaster australis, (Duncan) i — 1 



Pcntagonaster sp — 1 — 



Terebratulina catinuliformis, Tate 1 — 1 



Magasella compta, Sow 1 1 1 



Dimya dissimilis, Tate — 1 1 



Pecten hochstetteri, Zittel — 1 1 



Spondylus gaederopoides, McCoy — 1 1 



There is thus an aln>ost complete identity of fossil contents,, 

 and the beds are on the same horizon. 



