Crocidolite is the asbestiform variety of riebeckite, known for its distinct deep blue, fibrous, and silky appearance. It occurs primarily in iron-rich metamorphic rocks and is famously the precursor for tiger's eye, where it is replaced by silica. Due to its toxicity as an amphibole asbestos, collectors should store it in sealed containers to prevent fiber inhalation.
Is this crocidolite?
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 crocidolite with a known reference. Crocidolite sits at Mohs 6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Crocidolite leaves a pale to bluish gray streak.
- 3Read the lusterHold the specimen under a strong light. Crocidolite typically shows a silky luster.
- 4Match the color rangeCompare against the expected color range: blue, lavender-blue, indigo.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous, asbestiform.
Often confused with
Crocidolite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Crocidolite leaves pale to bluish gray, Riebeckite leaves blue-gray; luster reads silky on Crocidolite and vitreous on Riebeckite.

How to tell apart: Streak differs, so Crocidolite leaves pale to bluish gray, Glaucophane leaves blue-gray; luster reads silky on Crocidolite and vitreous on Glaucophane.

How to tell apart: Crocidolite is noticeably harder (Mohs 6 vs. 2.5-3); streak differs, so Crocidolite leaves pale to bluish gray, Chrysotile leaves white.
Often found alongside crocidolite
Minerals reported to co-occur with crocidolite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂(Fe²⁺₃Fe³⁺₂)Si₈O₂₂(OH)₂
- Mohs hardness
- 6
- Density
- 3.2-3.4 g/cm³
- Colors
- Streak
- Pale to Bluish Gray
- Luster
- Silky
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous, Asbestiform
- Cleavage
- Perfect Prismatic
- Rarity
- Common
- Uses
- Collector
- Host rock
- Metamorphosed Banded Iron Formations
Where rockhounds find crocidolite
2 mapped spotsClassic worldwide localities
- Cape Province, South Africa
- Western Australia
- Bolivia
- Russia
Field-hunting tip
Look in metamorphosed banded iron formations country, the host setting where crocidolite typically forms. If you start seeing quartz, magnetite, hematite in float, you are in the right ground. Field specimens usually show a fibrous, asbestiform habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in California, Utah. Start trip planning there.



