Murashkoite is an extremely rare iron phosphide mineral originally discovered in the Kola Peninsula. It typically occurs as microscopic grains or inclusions within iron-rich environments associated with alkaline igneous rocks.
Is this murashkoite?
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 murashkoite with a known reference. Murashkoite sits at Mohs 5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Murashkoite leaves a gray streak.
- 3Read the lusterHold the specimen under a strong light. Murashkoite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: silver-white, gray.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: irregular grains, inclusions in other minerals.
Often confused with
Murashkoite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside murashkoite
Minerals reported to co-occur with murashkoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- FeP
- Mohs hardness
- 5-6
- Density
- 7.15 g/cm³
- Colors
- Streak
- Gray
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Irregular Grains, Inclusions in Other Minerals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Alkaline Igneous Rocks
- Typical price
- expensive based on rarity and research value
Where rockhounds find murashkoite
Classic worldwide localities
- Kola Peninsula, Russia
- Yenisei Ridge, Russia
Field-hunting tip
Look in alkaline igneous rocks country, the host setting where murashkoite typically forms. If you start seeing iron, troilite, graphite in float, you are in the right ground. Field specimens usually show a irregular grains, inclusions in other minerals habit, so train your eye for that shape before scanning the outcrop.





