u MEMOIRS OF THE QUEENSLAND MUSEUM. 
To Mr. H. A. Longman, Mr. B. Dunstan, Dr. F. W. Whitehouse, and 
Mr. A. N. Falk I wish to extend thanks for help in connection with the 
illustrations in this paper. 
SUMMARY. 
The Glenormiston meteorite, which weighed nearly 90 lb., may be 
regarded as a brecciated octahedrite of medium composition with a density 7-621. 
It is composed essentially of crystals of kamacite averaging approximately 
6 mm. in diameter and which are not orientated according to any definite 
arrangement as shown by their reflected surfaces, but which show well-developed 
Neumann lines after etching. 
Finite and plcssite occur as eutectic intergrowths with the kamacite 
crystals, while troilitc and schreibersite in the form of rounded or irregular 
nodules sometimes simple but often compound occur in moderate abundance. 
Widmanstatten structure is not present. 
