Migmatite is a composite rock formed under high-grade metamorphic conditions where partial melting occurs, creating distinct layers of light-colored granitic material and dark metamorphic rock. It displays a characteristic swirling or banded appearance known as migmatitic structure, often seen in high-grade regional metamorphic terrains. Collectors usually look for decorative polished slabs that highlight the complex interplay of light and dark mineral veins.
Is this migmatite?
4-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 migmatite with a known reference. Migmatite sits at Mohs 5-7 — softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Migmatite typically shows a vitreous luster.
- 3Match the color rangeCompare against the expected color range: black, white, gray, pink.
- 4Look at form & habitTypical habit: massive.
Often confused with
Migmatite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside migmatite
Minerals reported to co-occur with migmatite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 5-7
- Density
- 2.6-2.9 g/cm³
- Luster
- Vitreous
- Transparency
- Opaque
- Crystal habit
- Massive
- Cleavage
- None
- Rarity
- Common
- Uses
- Decorative, Construction, Architectural
- Host rock
- Deep Crustal Metamorphic Zones
- Typical price
- $5-50 for hand samples, higher for polished slabs
Where rockhounds find migmatite
Classic worldwide localities
- Finland
- Canada
- Norway
- Scotland
- United States
Field-hunting tip
Look in deep crustal metamorphic zones country — that is the host setting where migmatite typically forms. If you start seeing quartz, feldspar, biotite in float, you are in the right ground. Field specimens usually show a massive habit, so train your eye for that shape before scanning the outcrop.






