46 
Note-—A white, light-yellow, 
siliceous grains, overlies, in very 
in the neighborhood of Kyneton. Inter- 
entirely of very fine, 
Silurian rocks on the Coliban, 
stratified, thin beds of very coarse conglomer: 
but fossils seem to be entirely absent. 
ngs in Kyneton and the neighborhood. It 
frequently occur ; 
has been used in several buildi 
is soft and easily worked, but canno 
ugh it sometimes seems to harden 
and is, therefore, not a good building stone. 
large quantities ; and, tho 
it is very liable to exfoliate, 
The quarrie 
gold-bearing g 
overlies bot 
grit, numbers of la 
respective boundaries. 
20. SANDSTONE. Map No. Rd 36. 
Werribee, half a mile south of East 
Ballan. 3} sheet 11 S.W. 
Fine-grained, white freestone, similar 
to 19. 
21, YELLOW, GRITTY SANDSTONE. 
Hopkins’ River, 4 miles north of 
Hexham. 
22, MOTTLED YELLOW-AND- 
WHITE, GRITTY SANDSTONE. 
Coliban River, S.W. of Kyneton. 
4 sheet 9 S.W. » 
See No. 19 and Note. 
23. WHITE, SILICEOUS GRIT. 
List No. R (8) 
South Peak, Mount William, 
The grains of quartz appear to be 
cemented by felspathic matter. 
24, FLESH-COLORED, SILICEQUS 
Grit. List No. R (B) 
North Peak, Mount William. 
Resembles the last. 
25. Rep SANDSTONE. 
List No. R (i) 
North Peak, Mount William. 
26. LIGHT-RED QUARTZ GRIT. 
List No. R (E 
37, 
Mount Zero. — ) 
The grains cemented by felspathic 
matter. 
27. COARSE GRIT. 
Hopkins’ River, 4 miles north of 
Hexham. 
Very felspathic and uneven-grained, 
s are now abandoned. 
gravel beds overlie it in several places. 
h, seems to have caused an alteration into hard, coarse qu 
rge angular pieces of which are scattered round the 
PRIMARY OR PALASOZOIC ROCKS.—OASE X. 
often banded sandstone, composed 
thick beds, the 
ate, or pudding-stone, 
The sandstone 
t be procured of uniform color in 
on exposure, 
The Tertiary (Newer Pliocene) 
The basalt, which 
artz 
28, CLOSE-GRAINED, FINE GRIT. 
List No. R (3) 
North Peak, Mount William. 
29. Grirry CONGLOMERATE. 
List No. R (& 
Mount Timbertop. 
A reddish, coarse grit, with felspar 
and large pebbles of red sandstone. 
30. COARSE GRIT. 
Hopkins’ River, 4 miles north of 
Hexham. 
A white grit, with felspar. 
31. PINKISH-RED CONGLOMERATE. 
List No. R (Epi 
Mount Timbertop. 
An altered conglomerate of pink-and- 
yellow sandstone and quartz, with in- 
cluded pebbles, and a porphyritic cha- 
racter. 
32. BRECCIATED CONGLOMERATE. 
List No. R (A) 
71 
Base of Mount Timbertop. 
The oblong, rounded fragments all 
take parallel lines, and are much de- 
composed and oxidized. 
33. FINE-GRAINED, RED SAND- 
STONE. 
Summit of Mount Timbertop. 
34. Finz, Micacrous QUARTZ 
GRIT. 
Mount Tamboritta, Gippsland. 
