Moschellandsbergite is a rare silver-mercury amalgam found primarily in hydrothermal veins associated with mercury deposits. It typically occurs as small, silver-white dodecahedral crystals that quickly tarnish to a duller, yellowish-white surface upon exposure to air.
Is this moschellandsbergite?
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 moschellandsbergite with a known reference. Moschellandsbergite 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. Moschellandsbergite leaves a silver-white streak.
- 3Read the lusterHold the specimen under a strong light. Moschellandsbergite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: silver-white, pale yellow.
- 5Look at form & habitCrystal system: cubic. Typical habit: dodecahedral crystals, massive, granular.
Often confused with
Moschellandsbergite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside moschellandsbergite
Minerals reported to co-occur with moschellandsbergite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ag₂Hg₃
- Mohs hardness
- 3.5
- Density
- 13.5 g/cm³
- Colors
- Streak
- Silver-white
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Dodecahedral Crystals, Massive, Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Mercury-silver Veins
- Typical price
- $50-500 thumbnail
Where rockhounds find moschellandsbergite
Classic worldwide localities
- Moschellandsberg, Germany
- Almaden, Spain
- Rudnik, Serbia
Field-hunting tip
Look in hydrothermal mercury-silver veins country — that is the host setting where moschellandsbergite typically forms. If you start seeing cinnabar, mercury, silver in float, you are in the right ground. Field specimens usually show a dodecahedral crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.



