Terrywallaceite is a rare silver-lead-antimony sulfosalt mineral found in hydrothermal vein deposits. It is primarily identified in lab settings via electron microprobe analysis, appearing as small, opaque metallic grains within associated sulfide assemblages.
Is this terrywallaceite?
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 terrywallaceite with a known reference. Terrywallaceite 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. Terrywallaceite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Terrywallaceite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black, gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: anhedral grains, massive.
Often confused with
Terrywallaceite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside terrywallaceite
Minerals reported to co-occur with terrywallaceite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ag₃PbSb₃S₇
- Mohs hardness
- 2.5
- Density
- 6.85 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Anhedral Grains, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $100-500+ per specimen
Where rockhounds find terrywallaceite
Classic worldwide localities
- San Jose mine, Oruro, Bolivia
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where terrywallaceite typically forms. If you start seeing pyrite, quartz, galena in float, you are in the right ground. Field specimens usually show a anhedral grains, massive habit, so train your eye for that shape before scanning the outcrop.







