Holtedahlite is a rare magnesium phosphate mineral typically found as transparent to translucent tabular crystals or granular aggregates. It is primarily known from metasomatic zones within serpentinized ultramafic rocks and is a highly sought-after specimen for advanced mineral collectors.
Is this holtedahlite?
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 holtedahlite with a known reference. Holtedahlite sits at Mohs 4.5-5, 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: colorless.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, massive, granular.
Often confused with
Holtedahlite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside holtedahlite
Minerals reported to co-occur with holtedahlite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₁₂(PO₃OH,CO₃)(PO₄)₅(OH,O)₆
- Mohs hardness
- 4.5-5
- Density
- 2.94 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Tabular crystals, massive, granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a serpentine–magnesite deposit (Tingelstadtjern quarry, Norway); a common accessory mineral, of likely pneumatolytic origin, in an igneous magnetite–apatite deposit (Gole Gohar, Iran)
Where rockhounds find holtedahlite
Classic worldwide localities
- Tingelstadtjern quarry, Modum, Norway
- Into the millions of tons at the Gole Gohar iron deposit, Bafq district, Iran
Field-hunting tip
Where it forms: In a serpentine–magnesite deposit (Tingelstadtjern quarry, Norway); a common accessory mineral, of likely pneumatolytic origin, in an igneous magnetite–apatite deposit (Gole Gohar, Iran). If you start seeing althausite, szaibelyite, apatite in float, you are in the right ground. Typical habit: tabular crystals, massive, granular. Train your eye for that shape before scanning the outcrop.







