MINERALS OF QUEENSLAND. 253 
district ! !, with azurite (C.); Cloncurry !!!, frequent 
in “gossan ” often in large masses (L.); Cloncurry ! ! },. 
containing free gold; also pseudomorphs after cuprite, 
azurite and siderite (Q.M.C.); Great Australian 
Copper Mine, Cloncurry ! ! !, in large lode with native 
copper, cuprite, tenorite and azurite (J.); Bau Bau, 
Burnett district !, coating serpentine (Aplin) ; Taromeo, 
near Narrango (Q. M.C.); Curlew, about 12 miles 
south of Charters Towers !, with galena, gold quartz, 
chrysocolla and pyromorphite (C.); Burdekin River, 
near Mount Keelbottom ! !, in lode in quartz porphyry 
country (J.); Great Kennedy Copper Mine!!!, in a 
large lode, with azurite and cuprite (J.) ; Keelbottom 
Copper Mine ! !, IN quartz veins in porphyry (w.)3 
Mount Perry !!!, disseminated through granite (R.) ; 
Mount Perry district !!, in copper lodes, but not 
of very frequent occurrence (L.) ; Peak Downs Copper 
Mine, near Clermont! ! !, in fine botryoidal masses 
(L.); Mount Gotthard, near Lake Elphinstone, 100 
miles west of Mackay !!, in ‘“gossan” and in small 
veins (L.); Mount Orange Copper Mine ! !, with other 
copper ores (L.); Pine Vale, 25 miles south-west of 
Mackay ! !, massive, in reefs, and as stains in quartz,. 
also as an alteration product of copper pyrites (M). 
Massicot—Stanton Harcourt, Burnett district, from decomposing 
galena (R.); Argentine Silverfield !!!, (argentiferous), 
from decomposition of galena (J.) ; Dugald River ! !, in 
large lode, contains according to assays by K. T. Staiger, 
antimony and silver (J.); in small quantities at all the 
silver-lead mines ! ! (J.). 
MeExaconiteE—Great Australian Copper Mine, Cloncurry !, occa- 
sional crystals, with cuprite and native copper (J.) ; 
Great Kennedy Copper Mine !!, in a large lode, asso- 
ciated with azurite and malachite (J.) ; Ironclad Mine, 
Herberton !, with sulphates of iron and copper, and 
iron pyrites, hematite, &., &e. (C.); Mount Leyshon, 
17 miles south of Charters Towers !, with pyrites in the 
country rock of the mount; country rock has been 
identified by Mr. Jack, the Government Geologist, as a 
volcanic ash (C.); Pine Vale, 25 miles south-west of 
Mackay !, an alteration product of copper pyrites, in a 
quartzose matrix (M.); Blue Mountains, near Eton ! ! 
(J.); Emu Plains, Bowen River, mixed with argentite 
(J.); Mount Perry district ! !, with chalcopyr ite (L.) ; 
Texas, Stanthorpe district ! !, with other copper ores (G. ‘ 
Mercury — Kilkivan district !} in a hard, dark quartzose 
rock (R.). 
