Fig. 9. — Cyathaxoma- Beds at the Bathing-Place, north of Rush Bay. 



[The beds are nearly vertical, and two small thrusts are seen, hading in opposite 

 directions. The beds at the bottom of the cliff appear to have undergone 

 a greater amount of compression than the beds above, and thus have 

 produced the effect of thrusts in the upper beds.] 



Fig'. 10. — Cy&thaxoma-Limestones on the coast at Giant's Hill, 

 looking eastward. 



[The thinly-bedded limestones are nearly vertical. They are crossed by close 

 parallel joints dipping southward, which appear to be of the nature of 

 rough, imperfect cleavage-planes.] 



