Cookeite is a lithium-rich member of the chlorite group that typically forms as a coating or alteration product on other minerals like tourmaline. It is most often found as thin, pearly, micaceous aggregates or soft, pseudo-hexagonal plates in pockets of complex pegmatites.
Is this cookeite?
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 cookeite with a known reference. Cookeite sits at Mohs 2.5-3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: pearly or silky.
- 4Match the color rangeCompare against the expected color range: white, green, brown, yellowish white, pinkish white.
- 5Look at form & habitCrystal system: triclinic. Typical habit: micaceous, pseudo hexagonal.
Often confused with
Cookeite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside cookeite
Minerals reported to co-occur with cookeite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- LiAl₄(Si₃Al)O₁₀(OH)₈
- Mohs hardness
- 2.5-3.5
- Density
- 2.58-2.69 g/cm³
- Streak
- White
- Luster
- Pearly or silky
- Transparency
- Transparent to translucent
- Crystal system
- Triclinic
- Crystal habit
- Micaceous, pseudo hexagonal
- Cleavage
- {001}, perfect
- Rarity
- Uncommon
- Uses
- Collector, Mineralogical study
- Host rock
- A late-stage hydrothermal alteration product of lithium-bearing minerals in pegmatites; a primary hydrothermal vein mineral
Where rockhounds find cookeite
1 mapped spotsClassic worldwide localities
- Hebron, Mt. Mica, near Paris, and Buckfield, Oxford Co., Maine, USA
- Pala and Rincon districts, San Diego Co., California, USA
- Jeffrey quarry, North Little Rock, Pulaski Co., Arkansas, USA
- Waitabit Creek, northwest of Donald, British Columbia, Canada
- Ogofau, Carmarthenshire, England
- Radkovice and Dobrá Voda, Czech Republic
Field-hunting tip
Where it forms: A late-stage hydrothermal alteration product of lithium-bearing minerals in pegmatites; a primary hydrothermal vein mineral. If you start seeing lepidolite, spodumene, tourmaline in float, you are in the right ground. Typical habit: micaceous, pseudo hexagonal. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in California. Start trip planning there.







