Grumantite is a rare sodium-silicate mineral found primarily in the hyperalkaline complexes of the Kola Peninsula. It typically forms delicate bladed or fibrous white to colorless crystals, often appearing as radiating sprays within nepheline syenite pegmatites.
Is this grumantite?
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 grumantite with a known reference. Grumantite sits at Mohs 5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Grumantite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Grumantite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: bladed crystals, radiating aggregates, fibrous.
Often confused with
Grumantite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside grumantite
Minerals reported to co-occur with grumantite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaHSi₂O₅·H₂O
- Mohs hardness
- 5
- Density
- 2.44 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Bladed Crystals, Radiating Aggregates, Fibrous
- Cleavage
- Perfect On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hyperalkaline Igneous Rocks, Specifically Pegmatites
- Typical price
- $50-300 per specimen depending on size and crystal quality
Where rockhounds find grumantite
Classic worldwide localities
- Khibiny Massif, Kola Peninsula, Russia
- Lovozero Massif, Kola Peninsula, Russia
Field-hunting tip
Look in hyperalkaline igneous rocks, specifically pegmatites country — that is the host setting where grumantite typically forms. If you start seeing nepheline, microcline, aegirine in float, you are in the right ground. Field specimens usually show a bladed crystals, radiating aggregates, fibrous habit, so train your eye for that shape before scanning the outcrop.






