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. Ershovite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Ershovite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brownish-yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, radial aggregates.
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
- 2.58 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Radial Aggregates
- Cleavage
- Perfect On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find ershovite
Classic worldwide localities
- Khibiny Massif, Kola Peninsula, Russia
Field-hunting tip
Look in alkaline pegmatites country — that is the host setting where ershovite typically forms. If you start seeing natrolite, microcline, pectolite in float, you are in the right ground. Field specimens usually show a tabular crystals, radial aggregates habit, so train your eye for that shape before scanning the outcrop.






