Beusite-(Ca) is a rare phosphate mineral found primarily in complex granitic pegmatites. It typically occurs as brownish, massive to granular masses and is often chemically associated with other triphylite group members in advanced stages of pegmatite evolution.
Is this beusite-(ca)?
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 beusite-(ca) with a known reference. Beusite-(Ca) sits at Mohs 4-5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Beusite-(Ca) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Beusite-(Ca) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, yellow-brown, dark brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: massive, granular, or interstitial filling.
Often confused with
Beusite-(Ca) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside beusite-(ca)
Minerals reported to co-occur with beusite-(ca). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn²⁺Ca(PO₄)₂
- Mohs hardness
- 4-5
- Density
- 3.6-3.7 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Massive, Granular, Or Interstitial Filling
- Cleavage
- Distinct On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granitic Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find beusite-(ca)
Classic worldwide localities
- White Picacho district, Arizona, USA
- Mangualde, Portugal
- Hagendorf-Pleystein, Germany
- Tvedestrand, Norway
Field-hunting tip
Look in granitic pegmatites country — that is the host setting where beusite-(ca) typically forms. If you start seeing triphylite, apatite, quartz in float, you are in the right ground. Field specimens usually show a massive, granular, or interstitial filling habit, so train your eye for that shape before scanning the outcrop.







