Kentbrooksite is a rare silicate mineral belonging to the eudialyte group, characterized by its distinctive brown coloration and trigonal crystal symmetry. It is primarily found in highly alkaline igneous rocks like those in the Mont Saint-Hilaire region. Collectors prize it as a rare member of the eudialyte family, often occurring as small inclusions or grains within complex pegmatitic matrices.
Is this kentbrooksite?
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 kentbrooksite with a known reference. Kentbrooksite 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: yellowish brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: aggregates, anhedral grains.
Often confused with
Kentbrooksite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kentbrooksite
Minerals reported to co-occur with kentbrooksite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,REE)₁₅(Ca,REE)₆Mn₃Zr₃Nb(Si₂₅O₇₃)(O,OH,H₂O)₃(F,Cl)₂
- Mohs hardness
- 5-6
- Density
- 3.10 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Aggregates, anhedral grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In alkaline pegmatitic bodies cutting pulaskite
Where rockhounds find kentbrooksite
Classic worldwide localities
- Amdrup Fjord, Kangerdlugssuaq intrustion, East Greenland (type locality)
Field-hunting tip
Where it forms: In alkaline pegmatitic bodies cutting pulaskite. If you start seeing kupletskite, låvenite, catapleiite in float, you are in the right ground. Typical habit: aggregates, anhedral grains. Train your eye for that shape before scanning the outcrop.







