Tokkoite is a rare potassium-calcium silicate mineral found primarily in the alkaline rocks of the Murun Massif in Siberia. It typically appears as yellowish-brown fibrous or radiating aggregates and is often associated with the mineral tinaksite. Due to its limited distribution, it is highly sought after by systematic mineral collectors.
Is this tokkoite?
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 tokkoite with a known reference. Tokkoite sits at Mohs 5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Tokkoite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Tokkoite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, yellow-brown.
- 5Look at form & habitCrystal system: triclinic. Typical habit: fibrous, massive, radiating clusters.
Often confused with
Tokkoite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside tokkoite
Minerals reported to co-occur with tokkoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂Ca₄Si₇O₁₇(OH,F)₂
- Mohs hardness
- 5-6
- Density
- 2.9 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Fibrous, Massive, Radiating Clusters
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Rocks
- Typical price
- $20-150 for small specimens
Where rockhounds find tokkoite
Classic worldwide localities
- Tokko River, Murun Massif, Russia
- Chara-Tokko district, Siberia
Field-hunting tip
Look in alkaline igneous rocks country, the host setting where tokkoite typically forms. If you start seeing tinaksite, potassian richerite, aegirine in float, you are in the right ground. Field specimens usually show a fibrous, massive, radiating clusters habit, so train your eye for that shape before scanning the outcrop.




