Tetradymite is a distinct telluride mineral recognized by its metallic luster and perfect basal cleavage, often forming foliated, platy masses that resemble molybdenite. It is most commonly found in hydrothermal gold-bearing veins and contact metamorphic skarns. Collectors should look for its characteristic steel-gray color and sectile nature.
Is this tetradymite?
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 tetradymite with a known reference. Tetradymite 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. Streak: pale steel-gray.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic, splendent on fresh surfaces.
- 4Match the color rangeCompare against the expected color range: steel gray, yellow gray.
- 5Look at form & habitCrystal system: trigonal. Typical habit: granular, lamellar, pseudo hexagonal.
Often confused with
Tetradymite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Tetradymite leaves pale steel-gray, Molybdenite leaves bluish gray.

How to tell apart: Streak differs, so Tetradymite leaves pale steel-gray, Bismuthinite leaves lead-gray.

Often found alongside tetradymite
Minerals reported to co-occur with tetradymite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Bi₂Te₂S
- Mohs hardness
- 1.5-2
- Density
- 7.3 g/cm³
- Colors
- Streak
- Pale steel-gray
- Luster
- Metallic, splendent on fresh surfaces
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Granular, lamellar, pseudo hexagonal
- Cleavage
- Perfect on {0001}
- Rarity
- Uncommon
- Uses
- Collector, Ore of tellurium
- Host rock
- In hydrothermal gold-quartz veins of medium to high temperature of formation; also in contact metamorphic deposits
Where rockhounds find tetradymite
2 mapped spotsClassic worldwide localities
- Trail Creek, Blaine Co., Idaho, USA
- Sylvanite district, Hidalgo Co., New Mexico, USA
- Whitehall mines, Spotsylvania Co., Virginia, USA
- Žubkov (Schubkau) (type locality), as fine twinned crystals, Slovakia
- Băiţa (Rezbánya), also Ciclova, Moraviţa (Moravicza), and Oraviţa (Oravicza), Romania
- Narverud and Seljord, Norway
Field-hunting tip
Where it forms: In hydrothermal gold-quartz veins of medium to high temperature of formation; also in contact metamorphic deposits. If you start seeing tellurium, tellurobismuthite, gold in float, you are in the right ground. Typical habit: granular, lamellar, pseudo hexagonal. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in New Mexico, North Carolina. Start trip planning there.





