Garnet Schist is a metamorphic rock characterized by its distinct foliation and embedded porphyroblasts of garnet. Collectors prize specimens that display large, well-formed garnet crystals sitting prominently within a glittering, micaceous matrix.
Is this garnet 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 garnet schist with a known reference. Garnet Schist sits at Mohs 3-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Garnet Schist leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Garnet Schist typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: gray, brown, silver, dark red.
- 5Look at form & habitTypical habit: foliated.
Often found alongside garnet schist
Minerals reported to co-occur with garnet schist. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 3-7
- Density
- 2.7-3.2 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Opaque
- Crystal habit
- Foliated
- Cleavage
- Perfect Schistose Cleavage
- Rarity
- Common
- Uses
- Collector, Educational
- Host rock
- Regional Metamorphic Belts
- Typical price
- $5-30 per hand specimen
Where rockhounds find garnet schist
Classic worldwide localities
- Vermont, USA
- Scotland
- Norway
- Austria
- Switzerland
Field-hunting tip
Look in regional metamorphic belts country — that is the host setting where garnet schist typically forms. If you start seeing almandine, muscovite, biotite in float, you are in the right ground. Field specimens usually show a foliated habit, so train your eye for that shape before scanning the outcrop.




