272 Proceedings of the Royal Society of Victoria. 



lite. These minerals do not penetrate or mix with it, 

 as in the case of some meteorites. Cranbourne No. 1 

 Meteorite (F.), Beaconsfield Meteorite (C), Cranbourne 

 No. 2 and Langwarrin Meteorites (W.). 

 Analysis : 



Cranbourne No. 1 Beaconsfield 



I. 2. 3. 4. I. 2. 



Iron - - - _ - 62-150 - 63-613 - — - 57-49 - 58-08 



Nickel ----- 0-446 - — - _ - 4-30 - 4-34 



Cobalt ---—-—-—-— - 1-50 - 1-52 



Sulphur - - - 36-543 - — - 36-207 - 36250 - 35-71 - 36-07 



Copper . - - — - 0-079 - — - — . _ . _ 



Chlorine - - — - 0-130 - — - — - trace - — 



Graphite - - _ - __._-_ . o-33 - — 



Insol. residue - 0-215 - 2-297 - — -—-—- — 



TuRQUOis. — Hydrous phosphate of aluminium with some copper. 

 Thin veins and incrustations of greenish-blue colour with 

 quartz and slate, Lurg, near Benalla (M.Dt.). 

 Wolframite. — Iron and manganese tungstate. 



Crystals in quartz from the granite of Mount Buffalo ; sand 

 in an auriferous wash, foot of Mount Buffalo and 

 Hoddle's Creek; in quartz, Cameron's Creek; tabular 

 plates in quartz, Jenolan River, Mallacoota (W.). 

 Head of Boggy Creek, Bullumwaal; in wash, Ensay; as a 

 lode intermixed with quartz, Buckwong Creek, Lime- 

 stone Creek (CI.). 

 Analysis of Wolframite from Buckwong Creek (CI.) : 



Tungstic ti'ioxide - - 75*20 

 Manganese oxide - - 5-74 

 Ferrous oxide - - - 17-63 

 Insoluble residue (mainly silica) 1 -24 



