(Tr<(pfollte Beds at Dnylesford. 271 



Geoldc^ical Survey. Ho states that he has not noticed the per- 

 sistent westerly dip between the Loddon and Daylesford, re- 

 ferred to by Krause. He mentions several fossil localities, four 

 of which are marked on his map, but gives no further namea 

 except Hymenocaris. His map is published as quarter-sheet 

 16 N.E. 



The area to the south, of which the map is quarter-sheet 16 

 S.E., was surveyed by Mr. S. B. Hunter. The report is in Pro- 

 gress Report No. 9 of the Geological Survey. He mentions the 

 occurrence of graptolites, and states that both east and west of 

 the most folded belt there is a persistent dip to the west. 



Dr. T. S. Hall, in his paper on the Geolog}' of Castlemaine 

 (Proc. Royal Society of Victoria, Vol. VII., new series, 1895) 

 refers the only Daylesford fossils which he had then seen to the 

 zone of Tetragraptus frutioosus. Referring to this in a paper 

 dealing with othea* features of these rocks (Proc. Royal Society of 

 Viotoria, Vol. XIV., pt. 2, n.s.), I mention them as the lowest 

 parts of the Castlemaine series, meaning thereby the lowest parts 

 of the rocks which occur at Castlemaine, not the Castlemaine 

 series in the more limited sense in which that term is now com- 

 monly used. 



More recently Dr. Hall has identified other fossils from this 

 district (Records Geological Survey of Victoria, Vol. I., pt. 4, 

 1906, AVid Vol. II., pt. 1, 1907), of which the localities and 

 horizons are as follows : — 



Cornish line of reef (stated by Mr. E. J. Dunn tO' be from the 

 mullock heap at the Victoria Cornisih Engine Shaft, and probably 

 from the 966ft. level), at the top of the Bendigo series. 



The Springs, Daylesford, Bendigo horizon, 



BuUarto, Castlemaine horizon. 



From the Daylesford Gold Mine Tip, probably Bendigonian, 

 and othei's from the same locality, Wattle Gully Beds. Mr. W. 

 Baragwanath, jr., who collected these, considers that they were 

 both probably from material excavated in sinking from 400 to 

 500ft. 



From a shaft quarter mile south of the Cornish Co.'s new shaft, 

 Castlemaine series. 



From the north side of the Jubilee Lake, quarter mile east of 

 the railway, Upper part of the Castlemaine series. Mr. Barag- 



