
———— 




Fig. 1. 
{ 
Ee r eS a 
e = 5 3° Ss x R Ss ft 
% ad ot = = an s ; 
Ee * 5 Ss eis 49 
RSs Ff S Po ; 
Rak =x c e 8 : 2 
B34 ee ESE gf 
ae  S oes bs * 
: s = at Dunstan Plait 
= & S oxo Sa" a ~ ars = 
Nein * - = a a PBA SEZs 
, snes ae fas Se — SS 
Tertiary Sandstones & Clays “Vag Contorted Schists 
% Lacustrint 2 qe i al 
































































































































































































































































a a® + 
RES 
*Terrace-formation of the basins in the interior of the Province of Otago. The peaks in the distance are 
8000 feet high: at their base lies the Wanaka Lake.’—J. H. 


