Rongibbsite is a rare secondary lead-aluminum silicate mineral found in oxidized base metal deposits. It typically occurs as small, yellow, platy or micaceous crystals often associated with other lead-bearing minerals in hydrothermal environments.
Is this rongibbsite?
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 rongibbsite with a known reference. Rongibbsite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Rongibbsite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Rongibbsite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-orange.
- 5Look at form & habitCrystal system: triclinic. Typical habit: platy crystals.
Often confused with
Rongibbsite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside rongibbsite
Minerals reported to co-occur with rongibbsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₂Al₂Si₂O₁₀(OH)₄
- Mohs hardness
- 3.5
- Density
- 2.81 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Platy Crystals
- Cleavage
- Perfect On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Lead-zinc Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find rongibbsite
Classic worldwide localities
- Rongibbs mine, Arizona, USA
Field-hunting tip
Look in oxidized hydrothermal lead-zinc deposits country — that is the host setting where rongibbsite typically forms. If you start seeing quartz, cerussite, wulfenite in float, you are in the right ground. Field specimens usually show a platy crystals habit, so train your eye for that shape before scanning the outcrop.





