RELATIONSHIPS OF THE AUSTRALIAN CAINOZOIC SYSTEM. 
from this point to the junction bears the aspect of a rejuvenated 
stream, flowing in a deep, entrenched valley (see Fig. 16). The 
line of fault referred to passes almost due north and south 
Volicanie- : 
SCOTT a Sie 
| [aia , a 
ge Z —_ fiesr Sage —} we 
Limes fone ~ matvré valiey chee e } 
as — ie 4) H f 
onal gla hel Bik Al 
ees eee = | 
rE llesreigh an five aie me Pies. T= 
or == \ re-juvenalea Ie gre. — 
Srrteam 
Fig 1b, VALLev oF THE GRANGE BURN BErween HENTY'S AnD THE 
JUNCTION wiTr mUDOY CREEK 
cutting the Muddy Creek at MacDonald’s, 1 mile south of 
Forsyth’s (see sketch map Hig. 13). The effect of this fault is 
seen on the course of the Grange Burn below Forsyth’s, where 
the mature stream, after coming from Hamilton and flowing 
over Kalimnan strata (Fig. 17), taking a more northerly turn, cuts 
through high banks of polyzoal limestone resting on quartz por phyry, 
thence flows to the west for 20 chains, and then southward for another 
| Cad vq, Sheff s she ¢ 
mn <= EN f 
nS: = oO == (FS a 
“Resorted Katuman ~ a SS = 3 tr 
wih basaraas 7. 5 oS = 
es ——_— —_ a — 
qovlders— aa ee pee 
Z Se ee) eS =e eS ue 
<\ talimnan shell bet == SSS 
3 WakhpYNasSd- Niakica-— ae | saat = 2 hee 
5 Terebra and H Lena biopsis a 
pe ese ee: a = zie 
Xe pennies: inch Frown n Sandy elay~S — Ot 
—— SRI =~ 
Scel 
Sanus Ai roal (imeciene a beac 
Grange eel u : i 
Fig. 17, SECTION IN BANK OF GRANGE BURN OPPOSITE 
FoRSYTHS. 
20 chains, after which it follows its normal westerly course towards 
the Wannon. On the same area of uplift at Muddy Creek, starting 
from Clifton Bank, the Balcombian beds gently dip, with some 
slight undulations, towards MacDonald’s, but are still seen at a 
[ 46 ] 
