Physiography. Geology.] SUBANTARCTIC ISLANDS OF NEW ZEALAND. 



709 





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Fig. 3. — Southekn Side of Bay outside WESTiiRN Entkance to Caunley Hakbouk. 



The cliffs are composed of regular flows of basalt and beds of scoria. Over those in the foreground the seas pour 



during strong westerly gales. 



I'iG. 4. — Western Entrance to Caknley Hakbouk. 



