Borocookeite is a rare lithium-bearing silicate mineral belonging to the chlorite group, characterized by its inclusion of boron. It typically forms thin, micaceous plates or flaky aggregates within complex granitic pegmatites. Collectors look for it associated with other late-stage pegmatite minerals like tourmaline and albite.
Is this borocookeite?
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 borocookeite with a known reference. Borocookeite sits at Mohs 2-2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Borocookeite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Borocookeite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale pink.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy or micaceous aggregates.
Often confused with
Borocookeite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside borocookeite
Minerals reported to co-occur with borocookeite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Li₂Al₄(Si₃B)O₁₀(OH)₈
- Mohs hardness
- 2-2.5
- Density
- 2.7-2.8 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy or Micaceous Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
- Typical price
- $20-100 per specimen
Where rockhounds find borocookeite
Classic worldwide localities
- San Piero in Campo, Elba, Italy
- Mount Mica, Maine, USA
- Siberia, Russia
Field-hunting tip
Look in granite pegmatites country — that is the host setting where borocookeite typically forms. If you start seeing tourmaline, quartz, albite in float, you are in the right ground. Field specimens usually show a platy or micaceous aggregates habit, so train your eye for that shape before scanning the outcrop.






