Harkerite is a rare borosilicate mineral found in high-temperature contact metamorphic zones. It typically forms white to colorless dodecahedral crystals that closely resemble common garnet, requiring laboratory analysis to confirm its unique composition.
Is this harkerite?
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 harkerite with a known reference. Harkerite sits at Mohs 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: dodecahedral crystals, massive, granular.
Often confused with
Harkerite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Garnet is the harder of the two (Mohs 6.5-7.5 vs. 5).

How to tell apart: Harkerite is noticeably harder (Mohs 5 vs. 3).

How to tell apart: Scapolite is the harder of the two (Mohs 6 vs. 5).
Often found alongside harkerite
Minerals reported to co-occur with harkerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₄₈Mg₁₆[AlSi₄O₁₅(OH)]₄(BO₃)₁₆(CO₃)₁₆·2(H₂O,HCl)
- Mohs hardness
- 5
- Density
- 2.95-2.96 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Trigonal
- Crystal habit
- Dodecahedral crystals, massive, granular
- Cleavage
- None
- Fluorescence
- Weak dark red under LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In skarns in dolomitic limestones at the contact with granite (Camas Malag, Scotland); in volcanic ejecta (Alban Hills, Italy)
Where rockhounds find harkerite
Classic worldwide localities
- Camas Malag, near Broadford, Isle of Skye, Scotland
- Chersky Ridge, Tas-haiatah, northeastern Siberia, Russia
- Alban Hills, Lazio, Italy
- Nordmark, Sweden
Field-hunting tip
Where it forms: In skarns in dolomitic limestones at the contact with granite (Camas Malag, Scotland); in volcanic ejecta (Alban Hills, Italy). If you start seeing calcite, monticellite, diopside in float, you are in the right ground. Typical habit: dodecahedral crystals, massive, granular. Train your eye for that shape before scanning the outcrop.





