Ershovite is a rare silicate mineral found in the unique alkaline igneous rocks of the Khibiny Massif. It typically forms as delicate, translucent, tabular crystals or radial sprays within cavities of pegmatites.
Is this ershovite?
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 ershovite with a known reference. Ershovite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: olive green, brownish green, yellowish green.
- 5Look at form & habitCrystal system: triclinic. Typical habit: anhedral grains, fibrous.
Often confused with
Ershovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ershovite
Minerals reported to co-occur with ershovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₄K(Fe³⁺,Mn,Ti)Si₄O₁₀(OH)₂·4H₂O
- Mohs hardness
- 2-3
- Density
- 2.75 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Anhedral grains, fibrous
- Cleavage
- {100} and {010}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In unweathered ultra-agpaitic pegmatites in a differentiated alkalic massif
Where rockhounds find ershovite
Classic worldwide localities
- Mts. Rasvumchorr and Koashva, Khibiny massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In unweathered ultra-agpaitic pegmatites in a differentiated alkalic massif. If you start seeing orthoclase, nepheline, sodalite in float, you are in the right ground. Typical habit: anhedral grains, fibrous. Train your eye for that shape before scanning the outcrop.








