Chesterite is a very rare polysomatic mineral first discovered in the ultramafic rocks of Vermont. It is typically found as lamellar or fibrous masses and is often intergrown with anthophyllite, making visual identification difficult without laboratory analysis.
Is this chesterite?
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 chesterite with a known reference. Chesterite sits at Mohs 5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Chesterite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Chesterite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: dark brown, brownish-black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: fibrous, lamellar aggregates.
Often confused with
Chesterite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside chesterite
Minerals reported to co-occur with chesterite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Mg,Fe)₁₇Si₁₆O₄₄(OH)₂
- Mohs hardness
- 5-6
- Density
- 3.1-3.2 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Fibrous, Lamellar Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Rocks, Specifically Ultramafic Schists
- Typical price
- $20-150 per specimen depending on size and quality
Where rockhounds find chesterite
Classic worldwide localities
- Chester, Vermont, USA
- Tillotson Peak, Vermont, USA
Field-hunting tip
Look in metamorphic rocks, specifically ultramafic schists country — that is the host setting where chesterite typically forms. If you start seeing anthophyllite, talc, kyanite in float, you are in the right ground. Field specimens usually show a fibrous, lamellar aggregates habit, so train your eye for that shape before scanning the outcrop.





