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 2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: yellowish-white.
- 3Read the lusterHold the specimen under a strong light. Luster: pearly.
- 4Match the color rangeCompare against the expected color range: brown, gray, light gray.
- 5Look at form & habitCrystal system: amorphous. Typical habit: metamict, platy.
Often confused with
Gerasimovskite vs. its common look-alikes, and how to tell them apart in the field.
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
- MnTi₃Nb₂O₁₂·9H₂O
- Mohs hardness
- 2
- Density
- 2.52-2.58 g/cm³
- Colors
- Streak
- Yellowish-white
- Luster
- Pearly
- Transparency
- Semitransparent
- Crystal system
- Amorphous
- Crystal habit
- Metamict, platy
- Cleavage
- One direction, perfect, micaceous
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As a secondary mineral formed by the late-stage hydrothermal alteration of Nb–Ti minerals (possibly epistolite) within ussingite-bearing pegmatites, associated with alkaline intrusions
Where rockhounds find gerasimovskite
Classic worldwide localities
- Found on Mts. Punkaruaiv, Karnasurt, Nepkhe, and Alluaiv, in the Lovozero massif, Kola Peninsula, Russia
- Occurs at Nákâlâq, in the Ilímaussaq intrusion, Greenland
Field-hunting tip
Where it forms: As a secondary mineral formed by the late-stage hydrothermal alteration of Nb–Ti minerals (possibly epistolite) within ussingite-bearing pegmatites, associated with alkaline intrusions. If you start seeing ussingite, epistolite, steenstrupine in float, you are in the right ground. Typical habit: metamict, platy. Train your eye for that shape before scanning the outcrop.







