Ferdowsiite is an extremely rare silver-antimony-telluride sulfide mineral first discovered in the Kuh-e-Shah region of Iran. It typically occurs as microscopic anhedral grains associated with other sulfide minerals in epithermal vein deposits. Due to its extreme rarity, it is primarily of interest to advanced professional mineralogists and specialized systematic collectors.
Is this ferdowsiite?
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 ferdowsiite with a known reference. Ferdowsiite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ferdowsiite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Ferdowsiite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: gray, white.
- 5Look at form & habitCrystal system: triclinic. Typical habit: anhedral grains.
Often confused with
Ferdowsiite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ferdowsiite
Minerals reported to co-occur with ferdowsiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- AgSb₂Te₂S₄
- Mohs hardness
- 2
- Density
- 4.96 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Triclinic
- Crystal habit
- Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Epithermal Quartz Veins
- Typical price
- n/a
Where rockhounds find ferdowsiite
Classic worldwide localities
- Kuh-e-Shah, Iran
Field-hunting tip
Look in epithermal quartz veins country — that is the host setting where ferdowsiite typically forms. If you start seeing quartz, pyrite, stibnite in float, you are in the right ground. Field specimens usually show a anhedral grains habit, so train your eye for that shape before scanning the outcrop.





