Brinrobertsite is a rare silver-rich clay mineral found primarily in the oxidation zones of ore deposits. It is typically identified through analytical techniques like X-ray diffraction, as it appears as unassuming, dull, massive clay material to the naked eye.
Is this brinrobertsite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch brinrobertsite with a known reference. Brinrobertsite sits at Mohs 1-2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Brinrobertsite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Brinrobertsite typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: white, pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fine-grained, massive.
Often confused with
Brinrobertsite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside brinrobertsite
Minerals reported to co-occur with brinrobertsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ag,Pb)₀.₃(Si,Al)₄O₁₀(OH)₂·nH₂O
- Mohs hardness
- 1-2
- Density
- 2.4-2.6 g/cm³
- Colors
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Fine-grained, Massive
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Ore Deposits
- Typical price
- $50-200 per specimen
Where rockhounds find brinrobertsite
Classic worldwide localities
- Broken Hill (Australia)
Field-hunting tip
Look in oxidized ore deposits country, the host setting where brinrobertsite typically forms. If you start seeing quartz, cerussite, galena in float, you are in the right ground. Field specimens usually show a fine-grained, massive habit, so train your eye for that shape before scanning the outcrop.






