Carbokentbrooksite is a rare member of the eudialyte group primarily known from the alkaline igneous complex at Mont Saint-Hilaire. It typically occurs as small, dark brown equant crystals embedded in syenite pegmatites. Identification usually requires professional analysis due to its striking chemical similarity to other complex silicates in the eudialyte group.
Is this carbokentbrooksite?
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 carbokentbrooksite with a known reference. Carbokentbrooksite 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. Carbokentbrooksite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Carbokentbrooksite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: dark brown, reddish-brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: equant to tabular crystals.
Often confused with
Carbokentbrooksite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside carbokentbrooksite
Minerals reported to co-occur with carbokentbrooksite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,◻)₁₂(Na,Ce)₆Ca₆Mn₃Zr₃NbSi₂₅O₇₃(CO₃,OH)₃(H₂O)
- Mohs hardness
- 5-6
- Density
- 2.98 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Equant to Tabular Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Rocks
- Typical price
- $50-300 per specimen
Where rockhounds find carbokentbrooksite
Classic worldwide localities
- Mont Saint-Hilaire, Quebec, Canada
Field-hunting tip
Look in alkaline igneous rocks country — that is the host setting where carbokentbrooksite typically forms. If you start seeing aegirine, microcline, arfvedsonite in float, you are in the right ground. Field specimens usually show a equant to tabular crystals habit, so train your eye for that shape before scanning the outcrop.







