Arsenquatrandorite is an extremely rare sulfosalt mineral primarily found in polymetallic hydrothermal deposits. It is identified by its metallic, lead-gray appearance and distinct striations on prismatic crystals, requiring professional chemical analysis for definitive identification.
Is this arsenquatrandorite?
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 arsenquatrandorite with a known reference. Arsenquatrandorite 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. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: lead-gray, steel-gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic, striated, massive.
Often confused with
Arsenquatrandorite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside arsenquatrandorite
Minerals reported to co-occur with arsenquatrandorite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ag₁₇.₆Pb₁₂.₈Sb₃₈.₁As₁₁.₅S₉₆
- Mohs hardness
- 3.5
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic, striated, massive
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- hydrothermal veins
Where rockhounds find arsenquatrandorite
Classic worldwide localities
- Barika gold deposit, Sardasht, West Azerbaijan Province, Iran
Field-hunting tip
Where it forms: hydrothermal veins. If you start seeing stannite, arsenopyrite, galena in float, you are in the right ground. Typical habit: prismatic, striated, massive. Train your eye for that shape before scanning the outcrop.





