Four Treasures Reference Database
Record No. 2955

Gemmological features of rubies and sapphires from the Barrington volcano, Eastern Australia

Journal Article
Webb, G. (1997) Gemmological features of rubies and sapphires from the Barrington volcano, Eastern Australia. Australian Gemmologist, Vol. 19, No. 11, pp. 471–475.
Sinkankas/Born No.: NIS / NIB  |  RWHL
corundum, sources.12, Australia.12, , gems
Ruby is rare in Australia, but in the Barrington area of New South Wales, ruby and pink sapphire form up to 50% by weight of the gem corundum concentrate. These stones have Cr₂O₃ contents of 0.60–1.42 wt.% and FeO contents of 0.44–0.75 wt.%. They typically range from 2 to 6 mm in size and contain inclusions of spinel and liquid-filled fractures. Polysynthetic twinning is common and is often associated with inclusions of boehmite needles. On the basis of trace-element content, the Barrington corundum is divided into two distinct suites: one related to ruby and the other typical of eastern Australian sapphires. The ruby-containing corundum suite originated in a metamorphic environment, whereas the non-ruby suite has a magmatic origin. Both suites were brought to the surface by basaltic volcanism.