VIENNA UNIVERSAL EXHIBITION, 1873. 25
portion gave 7 ozs. 1 dwt. per ton. From Buchan, Gipps Land
Tin.
350 Black Oxide of Tin and Iron Pyrites. These minerals occur
on the faces of the specimens, which show sections of thin stanniferous veins. From the vicinity of Beech- worth
351 Tin Ore in decomposed granite. From Beechworth
352 Tin Ore. Obtained from the bed of the Koetong Creek,
upper Murray lliver
353 Stanniferous Washdirt. From the Koetong Creek, upper
Murray Kiver
354 Tin Ore, with wdiicli is associated Gold and Tourmaline.
From the bed of the Latrobe River
Copper.
355 Native Copper in Silurian Shale. The Copper occurs in
nearly all the faces of the joints and fissures of the rock, and especially where there are thin veins of quartz. It is probably derived from the decomposition of Copper Pyrites. There are traces of Oxide and Carbonate of Copper. Got from 500 feet in depth beneath the surface ; 30 feet of shale of a similar character to this sample have been cut through. The strike of the shale is about 20° west of north; it has scarcely any underlie. From the Flying Scud Mine, Mount Egerton 35G Green and Blue Carbonate of Copper. From the Thomson River Copper Mine, Gipps Land
Antimony.
357 Antimony Regulus. From Heathcote
358 Antimony, Native. From a lode at Maldon
359 Sulphide of Antimony. From Costerfield, near Heathcote
360 Sulphide and Oxide of Antimony. From Blackwood
361 Sulphide and Oxide of Antimony. From Balaclava Hill,
Whroo
362 Antimony Ore. From an auriferous lode. It was got at
70 feet beneath the surface; the average width of the vein was 12 inches, depth of the water level about 150 feet; the strike of the lode was north and south. From the Inifer Reef, Coy’s diggings, near Wliroo
363 Cervantite (Oxide of Antimony). From a lode at Coimadai
364 Oxide of Antimony. Broken from the reef at a depth of 50
feet from the surface. This is an antimony reef, and it strikes east and west. It is irregular in width, being sometimes as much as 2 feet and diminishing to a mere