Graptolitc Be<U <if hai/lcsford. 279 



35. — Lower down Kidd's Gully, north-east of the same shaft. 

 Tetragraptus fruticosus is doubtfully present. 



36. — A short, distance upstream from the junction of White- 

 field Gully and Kidd's Gully. A few fossils were obtained, among 

 which Didymograptus bifidus was most common. 



37.— In Spring Creek, at the mouth of Wild Cat Gully, Phyl- 

 lograptus typus Avas obser^-e-d. 



38. — Road cutting on the Hepburn Road west of Doctor's 

 Creek. I'hyllograptus typus. t, Tetragraptus biyonoides,t, and 

 sponge spicules,!. Horizon uncertain,!. 



A good series of sections are exposed from the locality 6 down- 

 stream to the junction of Spring Creek and thence up Spring 

 Creek and Woman's Gully. 



An a.nticlinG with a stroriir northerly pitch occurs a short dis- 

 tance east of 6, followed by a syncline with a similar pitch, and 

 another anticline. This syncline and anticline cross the creek 

 twice in the bend south-west of the Hepburn recreation ground, 

 and also cross Spring Creek just above its junction with Sailor's 

 Creek. 



39. — Close to the syncline west of the recreation ground. 

 Didymograptus bifidus. 



40. — On the we.st bank of the Creek, and west of the syncline, 

 and north-west of the recreation ground. T. fruticosus,!, Ben- 

 digonian.f. 



41. — On the west side of Sailor's Creek and opposite the 

 mouth of Spring Creek. Tetragraptus fruticosus. f, T. bryon- 

 oides,t, Phyllograptus typus, f, Didymograptus bifidus?,!, Clono- 

 graptus alinormis,!, Bendigonian uppermost zone,!. Rhinoptero- 

 caris maccoyi and other Crustacea are also present. Immediately 

 to the south there is considerable mixing of these slates with the 

 sandstones, giving something of the appearance of a conglo- 

 merate. 



As tiie pitch is northerly and the beds are near a syncline and 

 some distance north from the locality 6, they would be expected 

 to be somewhat newer, as is also indicated by the fossils. 



After the syncline and anticline already referred to as cross- 

 ing Spring Creek there is for some distance up that creek an 

 easterly dip. A syncline occurs before reaching the road, and an 

 anticline immediately east of the road embankment at Breakneck. 



