The cliffs here, as mentioned above, are more calcareous than 

 further north (especially the jutting points), where they are 

 mostly pink, purple, brown, or black shales, with bands of 

 quartzite, highly coloured by iron. It is by these quartzite bands 

 that the dip is most apparent, the shales showing stratification 

 lines very poorly. 



The following are the distances of the various distinctive 

 points of the coast from the Port Willunga Jetty, as measured 

 by cyclometer : — 



End of Miocene reef 

 End of thickly-clothed sandhills 

 Beginning of gravelly clays . . . 

 Appearance of Eocene rocks 

 Disappearance of Eocene rocks 

 Appearance of Cambrian 

 Disappearance of Cambrian and reappear- 

 ance of Eocene (here highly inclined) 

 Reappearance of Cambrian ... 

 Final disappearance of Eocene 

 End of Cambrian reef 



As mentioned before, fossils are very difficult to collect, owing 

 to their being nearly all in fragments. The following, however, 

 I have identified : — 



From the first Eocene bed (of low inclination) — 

 Cidaris sp. 



Lovenia Forbesii, Ten.- Woods. 

 Scutellina patella, Tate. 

 Fibularia gregata, Tate. 

 Anteclon pertusa, Tate, m.s. 

 Waldheimia sp. (indet.). 



From the second Eocene bed (of high inclination) — 

 Cidaris sp. 



Echinus Woodsii, Laube. 

 Lovenia Forbesii, Ten.- Woods. 

 Fibularia gregata, Tate. 

 Echinolampas posterocrassus, Gregory. 

 Pecten consobrinus, Tate. 

 Waldheimia sp. (indet.). 



Distance S. 



of Port Willunga Jetty. 



.. (say) 2 miles 







4 " 







4.1 « 



2 







5i « 







5J « 







6| " 





appear- 



6f " 



71 ec 



' 2 



7 5 u 

 ' 8 





Olxllt/Ll J 



Estimated 

 only. 



... 



81 " 

 °4 J 





