5 
e cliffs here, as mentioned above, are more calcareous than 
fatte north (especially the jutting points), where they are 
mostly xu purple, brown, or black shales, with bands of 
lines qr poor 
ollowing are the distances of the various distinctive 
pollità of the coast from the Port Willunga Jetty, as measured 
by cyclometer :— 
Distance S. of Port Willunga Jetty. 
End of Miocene reef .. (say) 2 miles 
End of thickly-clothed sandhills Li * 
Beginning of gravelly clays ... m. 44 
Appearance of Eocene rocks 54 * 
Disappearance of Eocene rocks 5g“ 
Appearance of Cam el 
Disappearanceof Cambrian and reappear- 
ance of Eocene (here ‚highly es 62 “ : 
Reappearance of Cambrian 74 " joe i n 
Final disappearance of Eocene oe T“ 7 
End of C 8l * 
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 et bed (of low inclination )— 
Cidaris sp. 
Lovenia Forbesii, pues Woods. 
Scutellina patella, Tat 
Fibularia gregata, Tato. 
Antedon pertusa, Tate, m.s. 
Waldheimia sp. (indet.). 
From the Sonn re bed (of high inclination)— 
ida 
hans Woodsii, Laube. 
Lovenia Forbesii, oes Woods. 
Fibularia gregata, 
Echinolampas posteroerassus, Gregory. 
Pecten consobrinus, 
Waldheimia sp. (indet.). 
———— >< 
