being the Remarkable Cave and the 
blowholes on Brown Mountain and at 
Half-Moon Bay. 
Coming to more recent times, nothing 
of interest is to be seen, except, per¬ 
haps, the immense sand dunes at Half- 
Moon Bay, formed from the debris of 
the surrounding sandstone cliffs, aided, 
perhaps, by the material brought by the 
westerly drift. Few shell mounds were 
to be seen, telling of unsuitable condi¬ 
tions for aboriginal life. 
wmnruLMuSFuM w Fi .r 0 U r W 
