Journal Royal Society of NS.W.Vol. XXX = 1896. “Plate Il. 
SSS 
Pera 
a emai 
‘2 I TIOTD. - — SS rarer 
rr I = 
0 ee 
———— 
Sora 
SSSSSy 
aa 
oe 
Ss 
SSS = = 
NE ER/ i 
Ee 
Opposite 16 mile mark from Sydney on Western Railway line N. S Wales, 
ey EEE CO ne OS 
JenolanCaves 2% Seg M! Victoria Ss _ LONGITUDINAL SECTION 
fm => 88! ‘ey j 
; 332 8 sei ces 2 . THROUGH 
Radiol S 6ey < ao Se M'Vict o 
tretines eee _ a BLUE beni & SYDNEY COALFIELDS 
é cs D Fe ae o > : 
SF FE cee ae 8 _ from Jenolan Caves to Edge of Continental Shelf 
x a 
4 
a3 s | ——N.S.W— 
i Re) Se ee 
ee g <) oa 
Ly Eg COLE aS) - 
aw Tee ws 3 qt a & ee au a 
“inttuded ed by Quartz porphyry | Sel: e Sia & = 
= 4 cS Q S ES B 
j = y BS : RES = eo $= 
as. Says ‘ : Sl i§ 38 88 AEs aS 
a si) ae 2 8 s #8 BS = 288 3s 
ei je een hea z s 8 5 28 S 5 ¢ = 
| aks a LP 3 ES cS gS _= gSe 5 
Datum HWM IS fa = bs & - S98 datum HWM. 2 
A= 0 6m. 7m. 10m. 15m. 20m. 28m. Am 4lm. 432m. Se ee — 
ERS AND oF = > 
— BSS SEES ie > seen UNE DE POS) 3 aap oem pe 
c See Lae pea ee 
Diagram 2 LONGITUDINAL SECTION Se 
ee ig Monoclinal flexure & old He 
‘ o r Channel. (Nepean?) ile 
s @ z zig 3 AT aserone HILL fig 
8 a ci —— Ae 
eS 3 : 3s: 2 BiLuE MOovuNTAINS HE : 
Sg 5 a 8 OS oe See fie segs 
; a . % ear g 3 ape Se ee eee ie Le f 
et SWS © a 4 ee S” 
> arn aa, GEIS LLD f . eS 
| ae Ses Eos Lon SSSA cage ioe: Be: Da ; wie 
‘ gs ee ZS Sp eee eee TE Ese Ce (ees 
. 3) 3 KS a Rae —— ‘ Ps, ifies LES g 
% ng : SE Se eee oe 
| : VIAL SS SES SKS << PM sae dees j 
al =) ; ! ee Ee Ss 
= See SS 
Small Expansion fold resulting from). ~~. =§ 
hydration and oxidation developing M SE 
into overthrust fault in Wanamatta Shales ([ ase ) AR [NE ae 
For fine of Section Ato B. see Plate /. 
NOTE 
In the text tt 1s Stated that ib is probable evidence of 
unconformity here, between SP Is and Silurian 
ssibly however the supposed Devonian Conglom- 
-erates belong to the Tras Pes Beds. 
H.£E.C. Robinson. Deit 
