RELATIONSHIPS OF THE AUSTRALIAN CAINOZOIC S YSTEM. 
— « “ 
polyzoal rock some calcisponges typical of the Janjukian, as well 
as a fine specimen of Thamnastraea sera, a fable Cape coral. At 
the locality, Ad 14, the reef of limestone before mentioned is seen 
to have been once continuous with the limestone band in the middle 
of the cliff, and thus forms part of an anticline with a steep pitch 
of 28° to the N. 21° W. These beds dip to the west at about 15°, 
and are succeeded by yellow and brown clays, in the former of wliich 
F W 
Cuff-Section 
S wowitsq ovEkwyi 
-sli p. 
i 50 YARC5 W. oF l\d il,Cu^>.EWiS: 
nq r ufF e>£o (JKooqtiT Tjown 
there is a band of earthy limestone nodules. The Janjukian beds 
are followed by extensive ash and tuff beds of a brown and yellow 
colour, which are here seen to have slipped en bloc from above 
down to shore level (Fig. 9). To see the relation of the volcanic 
tuffs and the basalt to the beds immediately succeeding, we have to 
go eastward to within 1 mile of Clifton Springs Hotel. There we 
(?) KXuiMMArS qRlTS RESTiHq or< ETRo"D £T> SORF*cE oF 
T3P\SA,uW 2)00 W. OF CUFFE HOO SE. ,CU FTo N SPRiisqS. 
have the bedded tuffs, agglomerate and basalt underlying the grit 
beds (Fig. 10). At the base of the grit beds there is a coarse pebbly 
deposit of quartz and metamorphosed rocks, but the bulk of the 
[ 38 ] 
