Goldschmidtite is a rare potassium gold telluride mineral discovered as inclusions within diamonds from the Koffiefontein pipe. It represents a unique geochemical signature of mantle conditions where gold and tellurium are trapped deep within the Earth's interior.
Is this goldschmidtite?
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 goldschmidtite with a known reference. Goldschmidtite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Goldschmidtite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Goldschmidtite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: silver-white.
- 5Look at form & habitCrystal system: cubic. Typical habit: anhedral to subhedral grains.
Often confused with
Goldschmidtite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Goldschmidtite is noticeably harder (Mohs 3.5 vs. 1.5-2); streak differs — Goldschmidtite leaves black, Sylvanite leaves gray.

How to tell apart: Streak differs — Goldschmidtite leaves black, Calaverite leaves yellowish-green.
Often found alongside goldschmidtite
Minerals reported to co-occur with goldschmidtite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KAuTe₄
- Mohs hardness
- 3.5
- Density
- 8.52 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Anhedral to Subhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Kimberlite
- Typical price
- very high, research grade material
Where rockhounds find goldschmidtite
Classic worldwide localities
- Koffiefontein mine, South Africa
Field-hunting tip
Look in kimberlite country — that is the host setting where goldschmidtite typically forms. If you start seeing diamond, phlogopite, enstatite in float, you are in the right ground. Field specimens usually show a anhedral to subhedral grains habit, so train your eye for that shape before scanning the outcrop.



