Grumiplucite is an extremely rare mercury bismuth selenide mineral first described from the Grumipluca mine in Italy. It typically occurs as microscopic inclusions within other sulfide minerals, making it a challenging and prized specimen for micromounters. Collectors should handle it with caution due to its mercury content.
Is this grumiplucite?
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 grumiplucite with a known reference. Grumiplucite sits at Mohs 1.5-2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Grumiplucite leaves a gray streak.
- 3Read the lusterHold the specimen under a strong light. Grumiplucite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: gray, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: microscopic grains.
Often confused with
Grumiplucite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside grumiplucite
Minerals reported to co-occur with grumiplucite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- HgBi₂Se₄
- Mohs hardness
- 1.5-2
- Density
- 8.5 g/cm³
- Streak
- Gray
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Microscopic Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- expensive due to rarity
Where rockhounds find grumiplucite
Classic worldwide localities
- Grumipluca, Italy
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where grumiplucite typically forms. If you start seeing cinnabar, pyrite, calcite in float, you are in the right ground. Field specimens usually show a microscopic grains habit, so train your eye for that shape before scanning the outcrop.





