Gerasimovskite is a rare hydrated niobium-titanium hydroxide mineral found primarily in alkaline igneous environments. It typically occurs as massive, dull brown coatings or earthy crusts and is challenging to identify without advanced chemical testing due to its inconspicuous appearance.
Is this gerasimovskite?
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 gerasimovskite with a known reference. Gerasimovskite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Gerasimovskite leaves a yellowish-white streak.
- 3Read the lusterHold the specimen under a strong light. Gerasimovskite typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: brown, yellowish-brown, yellow.
- 5Look at form & habitCrystal system: amorphous. Typical habit: massive, crusts, earthy aggregates.
Often found alongside gerasimovskite
Minerals reported to co-occur with gerasimovskite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Nb,Ti,Fe,Mn)(OH)₅·nH₂O
- Mohs hardness
- 3-4
- Density
- 2.8 g/cm³
- Streak
- Yellowish-white
- Luster
- Dull
- Transparency
- Opaque
- Crystal system
- Amorphous
- Crystal habit
- Massive, Crusts, Earthy Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Nepheline Syenite Pegmatites
- Typical price
- varies, generally sold as micro-specimen material
Where rockhounds find gerasimovskite
Classic worldwide localities
- Lovozero Massif, Russia
Field-hunting tip
Look in nepheline syenite pegmatites country — that is the host setting where gerasimovskite typically forms. If you start seeing eudialyte, aegirine, lomonosovite in float, you are in the right ground. Field specimens usually show a massive, crusts, earthy aggregates habit, so train your eye for that shape before scanning the outcrop.




