Tsikourasite is an extremely rare molybdenum nickel phosphide first described from the Othrys ophiolite complex in Greece. It typically occurs as microscopic anhedral grains associated with other rare phosphides within chromite ores.
Is this tsikourasite?
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 tsikourasite with a known reference. Tsikourasite sits at Mohs 4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Tsikourasite leaves a gray streak.
- 3Read the lusterHold the specimen under a strong light. Tsikourasite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: silver-white, gray.
- 5Look at form & habitCrystal system: cubic. Typical habit: anhedral grains.
Often confused with
Tsikourasite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside tsikourasite
Minerals reported to co-occur with tsikourasite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mo₃NiP
- Mohs hardness
- 4
- Density
- 6.8 g/cm³
- Colors
- Streak
- Gray
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Ophiolitic Chromitite
- Typical price
- very high (research specimen only)
Where rockhounds find tsikourasite
Classic worldwide localities
- Othrys ophiolite, Greece
Field-hunting tip
Look in ophiolitic chromitite country — that is the host setting where tsikourasite typically forms. If you start seeing chromite, pentlandite, nickel-phosphides in float, you are in the right ground. Field specimens usually show a anhedral grains habit, so train your eye for that shape before scanning the outcrop.



