276 T. S. Hart: 



19.- — From loose material here, Phyllograptus typus,t, Tetra- 

 graptus bryonoides,t, either Castlemainian or Bendigonian,t. 



20. — South Cornish Company's mullock heap, T. fruticosus,t, 

 Bendigonian. 



This anticline, like the previous one, has a southerly pitch. 



21. — West of the last mentioned anticline, in a gully north of 

 Smith's Cteek and independent of it. North-west of the south 

 shaft of the Victorian Cornish Co., Tetragraptus fruticosus, 

 Phyllograptus typus, Rhinopterocaris and small Crustacea. 



22. — East of the anticline last mentioned, north-east of 18 and 

 high up on the north side of Smith's Creek, in east dipping beds. 

 A trench had been cut along the next bed with the fossil bed on 

 its wall, so that large quantities of material were available. 

 Tetragraptus bryonoides,t, Didymograptus cf. nicholsoni,t, 

 Clonograptus flexilis?,t, Clonograptus spp,t, Phyllogi-aptus 

 typusf, age uncertain, probably Bendigonian,!. I noticed no 

 examples of either Tetragraptus fruticosus, Didymograptus bifi- 

 dus or D. caduceus. 



23. — A few fossils were noticed in slightly newer beds a short 

 distance down the hill from 22. 



It appears, therefore, that Bendigo Beds do reach the surface 

 on this anticline. I was formerly under the impression that they 

 did not, as my first Bendigonian fossils in this vicinity were all 

 from mine mullock heaps: 



24. — A loose block containing Tetragraptus fruticosus was 

 found on the Lake road, near the long tunnel. Its origin is 

 quite uncertain, owing to the great length of this tunnel, but in 

 in view of the southerly pitch of the anticline near the last 

 localities, Bendigo l)eds would scarcely be expected on the sur- 

 face near this tunnel on it. and there is no sign as yet detected 

 of their appearance further east. There is, of course, the possi- 

 bility that the tuimel workings have at their entrance re-handlod 

 shaft material, or thivt the block may have not come frum the 

 tunnel at all. 



Higher up Smitli"s Creek the dip is for some distance easterly 

 frcmi tho localities 18 and 22. A syncline with an anticline 

 quickly following on the east, appears, and further cast tlie bed- 

 rock is buried under basalt. 



East of the S.iuth Cornish shaft, an anticline is exposed both in 



