Glaucophane is a primary indicator mineral for high-pressure, low-temperature metamorphic conditions, often found in blueschist facies rocks. It typically forms long, slender prismatic or fibrous crystals with a distinctive blue or blue-grey coloration.
Is this glaucophane?
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 glaucophane with a known reference. Glaucophane sits at Mohs 6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: blue-gray.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to pearly.
- 4Match the color rangeCompare against the expected color range: blue, blue-gray, lavender, black, gray, bluish black, lavender blue, azure blue.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: columnar, granular, massive.
Often confused with
Glaucophane vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside glaucophane
Minerals reported to co-occur with glaucophane. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂(Mg₃Al₂)(Si₈O₂₂)(OH)₂
- Mohs hardness
- 6
- Density
- 3.08-3.22 g/cm³
- Colors
- Streak
- Blue-gray
- Luster
- Vitreous to pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Columnar, granular, massive
- Cleavage
- Perfect on {110}, intersecting at ~56° and ~124°; partings on {010}, {001}
- Rarity
- Common
- Uses
- Collector, Geological indicator
- Host rock
- Characteristic of the blueschist facies, in former subduction zones in mountain belts; in the greenschist facies and in eclogites that have undergone retrograde metamorphism
Where rockhounds find glaucophane
Classic worldwide localities
- Kodiak Islands, Alaska, USA
- Syra Island, Cyclades Islands, Greece
- St. Marcel, Val d'Aosta, and Piollore (Biella), Piedmont, Italy
- Anglesey, Wales
- Ubuzan, Aichi Prefecture, and Otakiyama, Tokushima Prefecture, Japan
Field-hunting tip
Where it forms: Characteristic of the blueschist facies, in former subduction zones in mountain belts; in the greenschist facies and in eclogites that have undergone retrograde metamorphism. If you start seeing crossite, chlorite, epidote in float, you are in the right ground. Typical habit: columnar, granular, massive. Train your eye for that shape before scanning the outcrop.







