Serendibite is an exceptionally rare borosilicate mineral prized by collectors for its deep blue to green-blue color. It typically forms in contact metamorphic zones where boron-rich fluids interact with carbonate rocks. Due to its scarcity and refractive indices, it is one of the most expensive and sought-after gems in the mineral world.
Is this serendibite?
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 serendibite with a known reference. Serendibite sits at Mohs 6.5-7, 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: blue, blue green, gray blue, light yellow, dark blue.
- 5Look at form & habitCrystal system: triclinic. Typical habit: granular, twinning common.
Often confused with
Serendibite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside serendibite
Minerals reported to co-occur with serendibite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₄(Mg₆Al₆)O₄[Si₆B₃Al₃O₃₆]
- Mohs hardness
- 6.5-7
- Density
- 3.42-3.52 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Granular, twinning common
- Cleavage
- Good on {010}, {001}; (010) ^ (001) ~66°
- Rarity
- Rare
- Uses
- Collector, Gemstone
- Host rock
- In skarns, affected by boron metasomatism, along the contact between carbonate rocks and granite, tonalite, or granulite
Where rockhounds find serendibite
Classic worldwide localities
- Johnsburg, Warren Co., Amity, near Warwick, Orange Co., and Russell, St. Lawrence Co., New York, USA
- New City quarry, three km south of Riverside, Riverside Co., California, USA
- Gangapitiya, near Ambakotte, Sri Lanka
- Melville Peninsula, Northwest Territories, Canada
- Tayozhnoye iron deposit, 550 km south of Yakutsk, Yakutia, Russia
- Handeni district, Tanzania
Field-hunting tip
Where it forms: In skarns, affected by boron metasomatism, along the contact between carbonate rocks and granite, tonalite, or granulite. If you start seeing diopside, spinel, phlogopite in float, you are in the right ground. Typical habit: granular, twinning common. Train your eye for that shape before scanning the outcrop.








