
Tintenbar Opal
Hydrated silica (SiO2·nH2O)
Rare precious opal from Tintenbar in northern New South Wales, Australia, occurring in volcanic basalt rather than sedimentary rock.
- Mohs hardness
- 5.5-6.5
- Color
- bright play-of-color, often in a basalt host
- Type
- gemstone
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Overview
Tintenbar Opal is a rare and historically notable opal from the Tintenbar area in the Northern Rivers region of New South Wales, Australia. Unusually for Australian opal, it occurs in volcanic basalt rather than the sedimentary rock of fields like Lightning Ridge and Coober Pedy.
The field produced bright precious opal in the late 19th and early 20th centuries but was small and is now largely worked out, making genuine Tintenbar opal scarce and collectible.
Its volcanic origin links it more closely to opal from places like Honduras and Ethiopia than to the famous Australian sedimentary fields, giving it a special place in opal history.
Formation & geology
Tintenbar Opal formed in cavities and vesicles within weathered basalt. Silica-rich water, released as the basalt broke down, percolated through the rock and deposited hydrated silica in gas bubbles and fractures.
This volcanic (basalt-hosted) setting contrasts with most Australian opal, which forms in Cretaceous sedimentary basins. The play-of-color still results from orderly stacks of uniform silica spheres diffracting light.
The deposition occurred at low temperatures during the weathering and alteration of the basalt, with silica concentrating in the rock's voids.
How to identify it
Identify Tintenbar opal as precious opal showing play-of-color, typically associated with a dark basalt host rather than light sedimentary matrix. Genuine provenance is largely established by historical documentation given its rarity.
Hardness is about 5.5-6.5, streak white, with conchoidal fracture. The basalt matrix is a useful contextual clue, distinguishing it from sedimentary Australian opal.
Look-alikes include other basalt-hosted opals such as Honduran black opal (also in volcanic matrix) and sedimentary Australian opal (in claystone or sandstone). The volcanic host and historical association distinguish true Tintenbar material, though it is rare enough that most specimens are in collections.
Uses & significance
Tintenbar Opal is primarily of collector and historical interest because of its rarity and unusual volcanic origin. Suitable pieces are cut as cabochons for jewelry, but most surviving material is in collections.
Like all opal it requires careful handling, protection from impact, heat, and dehydration. Its scarcity means genuine, provenanced specimens carry premium value.
Its significance lies in being one of the few historically mined basalt-hosted opal occurrences in Australia, making it notable in the geological and mining history of opal.
Frequently asked questions
What makes Tintenbar opal unusual?
It forms in volcanic basalt rather than the sedimentary rock that hosts most Australian opal, making it rare and geologically distinctive.
Where is Tintenbar?
Tintenbar is in the Northern Rivers region of New South Wales, Australia.
Is Tintenbar opal still mined?
No; the small field was largely worked out long ago, so genuine Tintenbar opal is scarce and mostly held by collectors.
What is Tintenbar opal compared to?
Its basalt-hosted, volcanic origin makes it more like Honduran or Ethiopian opal than the famous Australian sedimentary fields.
Tintenbar Opal guides
In-depth guides for identifying, valuing, and understanding Tintenbar Opal.
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