Kanemite is a rare hydrated sodium silicate mineral primarily found in evaporitic alkaline lake deposits. It typically forms delicate, white, platy, or micaceous aggregates that are easily dehydrated upon exposure to air.
Is this kanemite?
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 kanemite with a known reference. Kanemite 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. Kanemite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Kanemite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: platy crystals.
Often confused with
Kanemite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside kanemite
Minerals reported to co-occur with kanemite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaHSi₂O₅·3H₂O
- Mohs hardness
- 2
- Density
- 2.1 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy Crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Lake Sediments
- Typical price
- $20-100 thumbnail
Where rockhounds find kanemite
Classic worldwide localities
- Lake Chad, Chad
- Searles Lake, USA
- Soda Lake, USA
Field-hunting tip
Look in alkaline lake sediments country — that is the host setting where kanemite typically forms. If you start seeing magadiite, quartz, calcite in float, you are in the right ground. Field specimens usually show a platy crystals habit, so train your eye for that shape before scanning the outcrop.




