Sapphirine is a rare magnesium-aluminum silicate typically found in high-grade metamorphic terrains. Collectors prize it for its range of blue to greenish-blue hues, though it is usually opaque to translucent in most localities.
Is this sapphirine?
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 sapphirine with a known reference. Sapphirine sits at Mohs 7.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Sapphirine leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Sapphirine typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: blue, blue-green, green, gray, white, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, granular aggregates, massive.
Often confused with
Sapphirine vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside sapphirine
Minerals reported to co-occur with sapphirine. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Mg,Al)₈(Al,Si)₆O₂₀
- Mohs hardness
- 7.5
- Density
- 3.4-3.5 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Granular Aggregates, Massive
- Cleavage
- Poor/indistinct
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- High-grade Metamorphic Rocks Such as Granulites and Pelitic Schists
- Typical price
- $20-200 per specimen depending on crystal size and transparency
Where rockhounds find sapphirine
Classic worldwide localities
- Fiskenæsset, Greenland
- Val di Vara, Italy
- Madagascar
- Sri Lanka
- Wilson Lake, Canada
Field-hunting tip
Look in high-grade metamorphic rocks such as granulites and pelitic schists country, the host setting where sapphirine typically forms. If you start seeing sillimanite, cordierite, garnet in float, you are in the right ground. Field specimens usually show a tabular crystals, granular aggregates, massive habit, so train your eye for that shape before scanning the outcrop.







