PRIMARY OR PALASOZOIC ROCKS.—CASE X. 
85. Grirry Quartz CoNGLOME- 
RATE. 
Hopkins’ River, 4 miles north of 
Hexham, 
Contains pebbles of pinkish quartz, 
with felspar. 
36. CELLULAR, SILICEOUS Rock. 
Stony or Moitun Creek, Dargo 
Road, Gippsland, 
The cavities are partially filled with 
brown clay. 
87. METAMORPHIC Rook. 
List No. R (&) 
Base of Mount Timbertop. 
Hackly, fractured, greenish 
brownish rock (hornfels). 
and 
38. Gritry CONGLOMERATE. 
Hopkins’ River, 4 miles north of 
Hexham. 
Same as No. 35, with large pebble of 
quartz and felspar porphyry. 
39. HARD, SLATY SHALE. 
List No. R (88) 
Beerjarg Camp, Broken River. 
40. CoNGLOMERATE. List No. R (Ñ) 
Mount Timbertop. 
Containing pebbles of indurated sand- 
stone, quartz, &c. 
4]. BRECCIATED CONGLOMERATE. 
List No. R (8) 
Mount Timbertop. 
Red, siliceous base, with quartz frag- 
ments and greenish altered sandstone. 
42. BRECCIATED CONGLOMERATE. 
List No. R (8) 
Mount Timbertop. 
Greenish rock, with quartz pebbles 
and green sandstone, 

47 
43. PEBBLE CONGLOMERATE. 
Map No. Rd 35. 
One mile and a half above Vic- 
toria Quarry, Korkuperrimul 
Creek. 4 sheet 11 S.E. 
Enclosing a piece of decomposed 
granite. 
44, FOSSILIFEROUS LIMESTONE. 
Buchan, Snowy River, S.E. Gipps- 
land, 
Hard, dark-grey, compactrock, afford- 
ing a good building lime. If mixed with 
the proper proportion of clayey matter, 
it would also form a good cement. 
The following is the result of an analysis 
by Mr. J. C. Newbery :— 

Carbonate of lime ... 87°72 
Rs iron 2°29 
5 magnesia 0°23 
Silica, clay, &c. Ary Xft 
97°85 
45. PEBBLY CONGLOMERATE 
SHALE. Map No. R (a 12), 
Mia-mia. 3 sheet 13 N.E. 
46. PEBBLY CONGLOMERATE. 
Map No. R (a 12). 
Same locality as the last. 
47. PEBBLY CONGLOMERATE. 
Map No. R (a12). 
Same locality as the last. 
48. PEBBLY CONGLOMERATE, 
$ List No. Rb 33B. 
Under Robertson’s Station, Wild 
Duck Creek, near Heathcote, 
49. YELLOW SANDSTONE. 
List No, Rb 338. 
i Same locality as the last. 
Occurs at the base of the pebble con- 
glomerate, 
50. GREENISH-BROWN GRIT. 
List No. Rb 33n. 
Under Robertson’s Station, Wild 
Duck Creek, near Heathcote. 
The formation, from which specimens 45, 46, and 47 are taken, is 
an extension of the beds occurring at the Wild Duck Creek, near 
Heathcote (specimens 48, 49, and 50), and: probably either the base of 
the Carbonaceous series or the top of the Upper Paleozoic beds; but 
fossils not having been discovered, its exact age is somewhat doubtful. 
Specimens Nos. 45, 46, and 47 were taken from a hole sunk by the 

