Saddlebackite is a rare lead-bismuth telluride mineral typically found as small grains within hydrothermal gold-bearing deposits. It is best identified through polished section microscopy or X-ray diffraction due to its similar physical appearance to other bismuth tellurides.
Is this saddlebackite?
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 saddlebackite with a known reference. Saddlebackite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Saddlebackite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Saddlebackite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: lead-gray.
- 5Look at form & habitCrystal system: trigonal. Typical habit: anhedral grains, inclusions.
Often confused with
Saddlebackite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside saddlebackite
Minerals reported to co-occur with saddlebackite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₂Bi₂Te₂S₃
- Mohs hardness
- 2.5
- Density
- 8.5 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Anhedral Grains, Inclusions
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Quartz Veins
- Typical price
- $50-300 per specimen
Where rockhounds find saddlebackite
Classic worldwide localities
- Saddleback, New South Wales, Australia
Field-hunting tip
Look in hydrothermal quartz veins country — that is the host setting where saddlebackite typically forms. If you start seeing gold, tellurobismuthite, pyrite in float, you are in the right ground. Field specimens usually show a anhedral grains, inclusions habit, so train your eye for that shape before scanning the outcrop.






