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, 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.





