234 MINERAL CENSUS OF AUSTRALASIA. 
ActTINOLITE—Cloncurry !, on calcite (Q.M.C.); Mount Perry 
district !!!, actinolite rock, and as green radiating 
crystal in actinolite rock (R.); Charters Towers !, in 
“Day Dawn Extended” quartz reef (J.), also in 
country rock (syenite) of ‘ North Australian Block,” 
(C.). 
Acate—Agate Creek, Etheridge! !, in large quantities (L.) ; 
Burnett district !!, over a wide area (N. Bartley) ; 
Narrango district ! ! (R.) ; Mount Toussaint and Mount 
Macedon !!, in geodes in epidote rock (J.); Agate 
Creek, Gilbert !! !, occurring “in thousands of tons ” 
in river gravels (4J.). 
AmMALGAM— Kilkivan, in hard dark quartzose rock (R.). 
Amertuyst—Logan River ! (R.); Upper Coomera, Albert district 
(R.) ; Cloncurry (Upper Camp 2) !, in alluvial (C.). 
ANALCIME—Strathmore Creek and Bowen River ! !, in geodes in 
epidote rock (J.). 
ANGLESITE—Silver Hill Mine, Mount Albion !, transparent 
pyramidal crystals (J.); at all the silver-lead mines, 
especially Argentine, Dry River, and Mount Albion ! ! !, 
argentiferous, enveloping argentiferous galena, and 
apparently derived from its decomposition (J.). 
ARGENTITE—Cumnor Lease, Silverfield, Tinaroo district—“ It 
is probable that in argentiferous galena from here, 
assaying 1400oz. silver to the ton, a good deal of this. 
silver is distributed through the galena in the form of 
free sulphide” (C. I. E.); Emu Plains, Bowen River, 
intimately mixed with cuprite and tenorite, especially 
the latter, the mixed ore containing 2299o0z. silver per 
ton (J.). 
He meeroreMicnnt Wheeler, 18 miles from Rockhampton ! !, in 
serpentine (D.) and (C.) ; Cloncurry !, in “ The Contra ” 
copper lode; near Gympie !, in serpentine (R.) ; 
Gympie !, with quartz in reefs (R.); Woodonga ! !, 
Glastonbury, Wide Bay district, in serpentine (R.) ; 
Mount Alma, Charters Towers ! !, in diorite rock, the 
vein cropping out at surface from 4in. to 5in. thick (C.) 
—perfectly white and silky in part, but bulk stony : 
silky portion lost no weight on treatment with warm 
hydrochloric acid, and was unaltered by blow-pipe or 
Bunsen flame (C.). 
AspouitE—Kilkivan, in a lode running nearly N. and S. in 
light-coloured serpentine, occurs sometimes in solid 
veins, sometimes in large botryoidal masses, but gene- 
rally running in an irregular manner through the 
