MINERALS OF QUEENSLAND. 235 
gangue (R.), [Analyses: undressed ore, Co 7:50 per 
cent., Ni 2°12 per cent., (K. T. Staiger) ; fair sample of 
lode, Co 7:50 per cent., Ni 2-25 per cent., Mn 18-00 per 
cent., (K. T. Staiger) ; surface ore, Co 2°75 per cent., 
Ni 2:25 per cent., Mn 65-00 per cent. (W. Vivian and 
Sons, Swansea).]; Kilkivan !!!, believed to be from 
lode referred to by (R.) ; “specimens of asbolite from 
same locality in Queensland Museum, where it is termed 
cobaltiferous wad, have the following assays appended : 
—Cobalt 22-207 per cent., nickel 3-510 per cent, iron 
29:130 per cent., manganese 2°360 per cent., copper 
0:103 per cent. (Cat. C.J. E.); Mountain Home !, in 
copper lode, associated with green carbonate of copper, 
ferruginous red oxide of copper, pyrolusite and garnets 
(J.). 
AtTAcAmiITE—Mount Perry district (Q. M. C.) ; Cloncurry, pseudo- 
morphous after cuprite (Q. M. C.). 
AzuritE—Great Kennedy Copper Mine ! ! !, in rhombic prisms 
and pyramids and in radiating botryoidal masses in a 
large lode (J.) ; Keelbottom Copper Mine ! !, in quartz 
veins in porphyrite country (J.); Contra Lode, Clon- 
curry !, in large copper lode in diorite country (J.) ; 
Pumpkin Gully, Cloncurry !!, in ferruginous cup of 
copper lode (J.) ; Great Australian Copper Mine, Clon- 
curry ! !, in large lode with cuprite, native copper and 
malachite (J.); Ironclad Mine, Watsonville !!, with 
cassiterite and malachite (J.) ; Clan Ronald, Eureka 
Creek, Tinaroo ! !, with malachite and cassiterite, from 
20 feet below surface (C.); Mount Garnet, Tinaroo. 
district ! !, with malachite (C.) ; Peak Downs Copper 
Mine !, near Clermont, not so common as malachite 
(L.) ; Mount Perry district !, with other copper ores (L.); 
Mount Orange Copper Mine, Nebo, accompanying mala- 
chite, hematite and black oxide of copper (W. J. C. 
Adrian) ; Pine Vale, 25 miles S.W. of Mackay ! !, 
massive in reefs, also as alteration product of copper 
pyrites, associated with quartz, zinc-blende, malachite, 
galena and quartz (M.). 
Barytes—Three miles from Mary River along Kilkivan Road ! ! !, 
as a large vein (R.) ; near Miva, Wide Bay ! ! (G.) ; 30 
miles west of Milo Station, near Adavale ! !, also 
Maxwelton, near Hughenden !, as radiated nodules in 
shales of the Rolling Downs (cretaceous) formation (J.). 
BismutH—Narrango !, in auriferous lode in a matrix of steatite 
(L.) ; Mount Biggenden, Degilbo, Wide Bay district ! ! !, 
(R.) ; Stanthorpe, in tin-wash (Q. M.C.); Pumpkin 
Gully, Cloncurry !!, in auriferous drift (J.); Mary. 
