Staurolite Schist is a medium-grade metamorphic rock characterized by the presence of cruciform or prismatic staurolite crystals embedded within a mica-rich matrix. It is highly sought after by collectors for the 'fairy cross' habit of the staurolite porphyroblasts, which often stand out clearly against the schistose background. It is typically found in regional metamorphic terranes formed under moderate temperatures and pressures.
Is this staurolite schist?
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 staurolite schist with a known reference. Staurolite Schist sits at Mohs 3.5-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Staurolite Schist leaves a white to gray streak.
- 3Read the lusterHold the specimen under a strong light. Staurolite Schist typically shows a pearly to dull luster.
- 4Match the color rangeCompare against the expected color range: dark brown, gray, brownish-black.
- 5Look at form & habitTypical habit: foliated matrix with embedded prismatic crystals.
Often found alongside staurolite schist
Minerals reported to co-occur with staurolite schist. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 3.5-7
- Density
- 2.7-3.0 g/cm³
- Streak
- White to Gray
- Luster
- Pearly to Dull
- Transparency
- Opaque
- Crystal habit
- Foliated Matrix with Embedded Prismatic Crystals
- Cleavage
- None
- Rarity
- Common
- Uses
- Collector, Educational
- Host rock
- Metamorphic Belts
- Typical price
- $5-50 thumbnail, $20-150 cabinet specimen
Where rockhounds find staurolite schist
Classic worldwide localities
- Taos County, New Mexico, USA
- Fannin County, Georgia, USA
- Brittany, France
- Ticino, Switzerland
- Minas Gerais, Brazil
Field-hunting tip
Look in metamorphic belts country — that is the host setting where staurolite schist typically forms. If you start seeing staurolite, muscovite, biotite in float, you are in the right ground. Field specimens usually show a foliated matrix with embedded prismatic crystals habit, so train your eye for that shape before scanning the outcrop.





