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. Tetradymite leaves a lead-gray streak.
- 3Read the lusterHold the specimen under a strong light. Tetradymite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: steel-gray, silver-white.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, foliated masses, bladed.
Often confused with
Tetradymite vs. its common look-alikes, and how to tell them apart in the field.
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
- 7.2-7.5 g/cm³
- Colors
- Streak
- Lead-gray
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Tabular Crystals, Foliated Masses, Bladed
- Cleavage
- Perfect Basal
- Rarity
- Uncommon
- Uses
- Collector, Ore of Tellurium
- Host rock
- Hydrothermal Veins, Contact Metamorphic Deposits
- Typical price
- $20-150 thumbnail
Where rockhounds find tetradymite
2 mapped spotsClassic worldwide localities
- Cheleken Peninsula, Turkmenistan
- Schmiedefeld, Germany
- Montgomery County, North Carolina, USA
- Berezovskoye, Russia
- Red Cloud Mine, Arizona, USA
Field-hunting tip
Look in hydrothermal veins, contact metamorphic deposits country, the host setting where tetradymite typically forms. If you start seeing gold, pyrite, chalcopyrite in float, you are in the right ground. Field specimens usually show a tabular crystals, foliated masses, bladed habit, so 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.







