Biotite is a common mica mineral known for its dark, plate-like appearance and perfect basal cleavage, which allows it to be peeled into thin, flexible sheets. It is a major constituent of igneous rocks like granite and is frequently found in metamorphic environments like gneiss and schist.
Is this biotite?
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 biotite with a known reference. Biotite sits at Mohs 2.5-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Biotite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Biotite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: black, dark brown, dark green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, massive, scaly aggregates.
Often confused with
Biotite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside biotite
Minerals reported to co-occur with biotite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K(Mg,Fe)₃(AlSi₃O₁₀)(OH,F)₂
- Mohs hardness
- 2.5-3
- Density
- 2.7-3.3 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Massive, Scaly Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Common
- Uses
- Industrial, Collector
- Host rock
- Igneous and Metamorphic Rocks Like Granite and Schist
- Typical price
- $2-20 for typical specimens
Where rockhounds find biotite
31 mapped spotsClassic worldwide localities
- Norway
- Canada
- USA
- Russia
- Greenland
U.S. states with biotite
Each link opens a state-specific list of mapped rockhounding spots that produce biotite.
Field-hunting tip
Look in igneous and metamorphic rocks like granite and schist country — that is the host setting where biotite typically forms. If you start seeing quartz, feldspar, hornblende in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, scaly aggregates habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Utah, Maine, Georgia — start trip planning there.







