Geology.] 



SUBANTARCTIC ISLANDS OF NEW ZEALAND. 



681 



portion 01 the coust-line between the north-east and south-east points, though two 

 small islands lie off this part, and two deep inlets — North-east Harbour and Per- 

 severance Harbour — strike far into the recesses of the island from the east. One 



III 



Gabbro. 





Miocene. 



1 



Ij^ 



Volcanic Breccia 





Volcanic Lavas. 



o 



Courrcjolles Point 



Yvon Villnrceaii 



25 North-east 

 Harbour 



Perseverance 

 20 Harbour 



Geologfical Map of 



CAMPBELL ISLAND. 



Scale of Nautical Miles. 



of the islets mentioned is situated at the north-east corner, and the other at the 

 entrance of the North-east Harbour. 



The south coast is far less regular. Here in several places the land falls pre- 

 cipitously from a level of 1,500 ft. high to the sea-margin, though the highest cliffs 



