Schachnerite is a rare silver-mercury amalgam typically found as microscopic grains or intergrowths within mercury-rich deposits. It is best identified through laboratory analysis of its metallic, silver-white appearance in specialized hydrothermal mineral assemblages.
Is this schachnerite?
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 schachnerite with a known reference. Schachnerite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: metallic.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: silver gray.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: anhedral grains, microscopic inclusions.
Often confused with
Schachnerite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Luster reads metallic on Schachnerite and bright metallic on Moschellandsbergite.

How to tell apart: Streak differs, so Schachnerite leaves metallic, Silver leaves silver-white.
Often found alongside schachnerite
Minerals reported to co-occur with schachnerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ag₁₁.₀-₁.₁Hg₀.₉-₁.₀
- Mohs hardness
- 2-3
- Density
- 13.52 g/cm³
- Colors
- Streak
- Metallic
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Anhedral grains, microscopic inclusions
- Cleavage
- Indistinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Found in the zone of oxidation, formed by the alteration of moschellandsbergite
Where rockhounds find schachnerite
Classic worldwide localities
- Vertraun Gott mercury mine at Landsberg, near Obermoschel, Rhineland-Palatinate, Germany
- Sala, Viistmanland, Sweden
Field-hunting tip
Where it forms: Found in the zone of oxidation, formed by the alteration of moschellandsbergite. If you start seeing paraschachnerite, mercurian silver, acanthite in float, you are in the right ground. Typical habit: anhedral grains, microscopic inclusions. Train your eye for that shape before scanning the outcrop.





