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
30 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, 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, Wisconsin. Start trip planning there.







