Mylonite is a fine-grained, cohesive metamorphic rock formed by intense ductile deformation in shear zones deep within the Earth's crust. It is characterized by a strong foliation or lineation, often containing rotated porphyroclasts of harder minerals like feldspar within a fine-grained matrix. Collectors often look for these in tectonically active zones where rocks have been significantly crushed and sheared under high pressure.
Is this mylonite?
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 mylonite with a known reference. Mylonite sits at Mohs 5-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Mylonite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Mylonite typically shows a dull to silky luster.
- 4Match the color rangeCompare against the expected color range: gray, black, white, brown.
- 5Look at form & habitTypical habit: fine-grained, foliated, mylonitic texture.
Often confused with
Mylonite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside mylonite
Minerals reported to co-occur with mylonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 5-7
- Density
- 2.6-2.8 g/cm³
- Streak
- White
- Luster
- Dull to Silky
- Transparency
- Opaque
- Crystal habit
- Fine-grained, Foliated, Mylonitic Texture
- Cleavage
- None
- Rarity
- Common
- Uses
- Geological Study, Educational
- Host rock
- Ductile Shear Zones
- Typical price
- $5-20 hand specimen
Where rockhounds find mylonite
Classic worldwide localities
- Moine Thrust Zone (Scotland)
- San Andreas Fault (USA)
- Alpine Fault (New Zealand)
- Norway
- Himalayas
Field-hunting tip
Look in ductile shear zones country — that is the host setting where mylonite typically forms. If you start seeing quartz, feldspar, mica in float, you are in the right ground. Field specimens usually show a fine-grained, foliated, mylonitic texture habit, so train your eye for that shape before scanning the outcrop.





