Britvinite is a rare lead-magnesium silicate mineral typically found as small, thin platy crystals in hydrothermal environments. It is primarily known from the Korchinskoye deposit in Russia, where it occurs alongside lead sulfides and carbonates.
Is this britvinite?
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 britvinite with a known reference. Britvinite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Britvinite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Britvinite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, radial aggregates.
Often confused with
Britvinite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside britvinite
Minerals reported to co-occur with britvinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₄Mg(Si₂O₇)(OH)₂
- Mohs hardness
- 3-4
- Density
- 3.1 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Radial Aggregates
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $50-300 per specimen
Where rockhounds find britvinite
Classic worldwide localities
- Korchinskoye Pb-Zn deposit, Russia
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where britvinite typically forms. If you start seeing galena, cerussite, diopside in float, you are in the right ground. Field specimens usually show a platy crystals, radial aggregates habit, so train your eye for that shape before scanning the outcrop.





