Polekhovskyite is a rare molybdenum nickel mineral that forms bluish gray color euhedral crystals. It occurs in phosphide assemblages in severely altered, diopside microbreccia in pyrometamorphic rocks. Associated minerals include murashkoite, transjordanite and hematite. It was first described from Halamish wadi, southern part of the Hatrurim Formation, Negev Desert, Israel.
Is this polekhovskyite?
4-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 polekhovskyite with a known reference. Polekhovskyite sits at Mohs 5-6, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: metallic.
- 3Match the color rangeCompare against the expected color range: white, gray.
- 4Look at form & habitCrystal system: hexagonal. Typical habit: euhedral crystals.
Often confused with
Polekhovskyite vs. its common look-alikes, and how to tell them apart in the field.
All properties
- Chemical formula
- MoNiP₂
- Mohs hardness
- 5-6
- Density
- 6.626 g/cm³
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Euhedral crystals
- Rarity
- Rare
- Uses
- Scientific research
- Host rock
- pyrometamorphic rocks
Where rockhounds find polekhovskyite
Classic worldwide localities
- Dead Sea region, Israel
Field-hunting tip
Where it forms: pyrometamorphic rocks. If you start seeing negev desert, israel in float, you are in the right ground. Typical habit: euhedral crystals. Train your eye for that shape before scanning the outcrop.


