Chessexite is an extremely rare sulfate-bearing silicate mineral primarily known from the alkaline igneous complex at Mont Saint-Hilaire. It typically forms small, colorless to white tabular crystals in cavities of intrusive rocks, often requiring micro-mineral identification techniques for accurate confirmation.
Is this chessexite?
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 chessexite with a known reference. Chessexite 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. Chessexite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Chessexite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals.
Often confused with
Chessexite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside chessexite
Minerals reported to co-occur with chessexite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,K)₄Ca₂Al₆(Si₆O₂₀)(SO₄)₄·4H₂O
- Mohs hardness
- 2
- Density
- 2.44 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Rocks
- Typical price
- $50-200 per specimen
Where rockhounds find chessexite
Classic worldwide localities
- Mont Saint-Hilaire, Quebec, Canada
Field-hunting tip
Look in alkaline igneous rocks country, the host setting where chessexite typically forms. If you start seeing analcime, microcline, sodalite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.





