278 T. S. Hart : 



The anticline and syncline at the lower end of Smith's Creek 

 appear to converge to the north and spread apart to the south. 

 On the north bank of the Lake two anticlines are probably pre- 

 sent corresponding to those at 19, and perhaps 25. An anti- 

 cline occurs at the Woodbum siding, exjDosed in a drain near the 

 road crossing. A syncline occurs at the north end of the big 

 bank to the south, and the big cutting beyond shows an anti- 

 cline and syncline. Fossils Avere obtained at several places. 



26, 27. — In the two cuttings between the Lake and Woodburn. 

 Only Tetragraptus serra from one of these, and Phyllograptus 

 typus from the othei*, were recognised. 



28. — At one of the mullock heaps of the Rising Star (now Vic- 

 torian Star) mine. Phyllograptus typus and Tetragraptus fruti- 

 cosus. The shaft is 750 i&&i deep, and they are probably from 

 the lowest workings. 



29. — In the bed of the Creek above the big embankment 

 south of Woodburn, a few fossils were noticed, but were inde- 

 cisive as to the horizon of the beds. 



30, 31, 32.— Three localities in the big cutting. At all of 

 these Didymograptus bifidusf is by far the most abundant fossil. 

 In addition there are Tetragraptus biyonnidesf and Phyllo- 

 graptus typusf at 30 and 32, and T. quadribrachiatusf at 32. 



30. — At the north end of the cutting east of the anticline. 



31. — Beyond the anticline, but before the syncline. 



32.— -Near the south end of the cutting, west of the syncline. 



These are all near the same horizon, and the same bed may be 

 repeated. All are Wattle Gully Beds. 



This anticline seemg to be most probably the same as passes 

 west of 11. No Bendigo Beds are exposed in the cutting, but 

 their disappearance is in accordance with the consistent southerly 

 pitch seen on the anticlines and synclines as before mentioned. 

 If the identification of the anticline is con-ect, one anticline and 

 one syncline seem to disappear southward fmm the series before 

 described. 



33. — A few fossils were obtained in Wnmbat Creek, a little 

 above the Lake Road Bridge. Their horizon was uncertain, but 

 the beds are probably the same as at 17. 



34. — In Kidd's Gully east of the Daylesford Co.'s shaft, one 

 small Didymograptus caduceus. 



