160 THE KORALEIGH STONY METEORITE 
more or less idiomorphic crystals up to 0°02 mm. in diameter. It 
is grey-brown in reflected light, isotropic, and inert to standard 
etching reagents. The small crystals sometimes occur as groups 
within a single grain of the silicate minerals. 
CONCLUSION 
The aerolite from Koraleigh, in New South Wales, is a bronzite- 
olivine chondrite like that from Caroline, on the Glenelg River 
near the Victorian-South Australian border. Because of the close 
similarity of these two aerolites in the various characteristics 
examined, it is thought probable that they may have close genetic 
relationships, and might even be portions of the same fall, as the 
Caroline aerolite was found at the site of a blackfellows’ camp, 
and had therefore possibly been transported from its original place 
of fall. 
REFERENCES 
1941 Baker, G., and Edwards, A. B. The Bond Springs Stony Meteorite. Mem. 
Nat. Mus., Melbourne, no. 12, pp. 49-58, 1941. 
1941 Stillwell, F. L. The Caroline Stony Meteorite. Mem. Nat. Mus., Mel- 
bourne, no. 12, pp. 41-48, 1941. 
Brown, Prior, Anderson Pty. Ltd. 
