Clinoenstatite is the monoclinic high-temperature polymorph of enstatite, often found in meteorites and specialized geological environments. It typically occurs as white or colorless prismatic crystals or granular masses and is notoriously difficult to distinguish from its orthorhombic counterpart, enstatite, without X-ray diffraction. Collectors value it primarily for its scientific significance as a component of extraterrestrial and mantle-derived materials.
Is this clinoenstatite?
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 clinoenstatite with a known reference. Clinoenstatite 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. Clinoenstatite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Clinoenstatite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, gray, colorless, pale green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, granular, massive.
Often confused with
Clinoenstatite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside clinoenstatite
Minerals reported to co-occur with clinoenstatite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- MgSiO₃
- Mohs hardness
- 5-6
- Density
- 3.2-3.3 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Granular, Massive
- Cleavage
- Good in Two Directions
- Rarity
- Rare
- Uses
- Collector, Research
- Host rock
- Metamorphic Rocks, High-temperature Volcanic Rocks, Meteorites
- Typical price
- $20-100 for small research-grade specimens
Where rockhounds find clinoenstatite
Classic worldwide localities
- Japan
- Germany
- USA
- meteorites
Field-hunting tip
Look in metamorphic rocks, high-temperature volcanic rocks, meteorites country — that is the host setting where clinoenstatite typically forms. If you start seeing forsterite, diopside, chromite in float, you are in the right ground. Field specimens usually show a prismatic crystals, granular, massive habit, so train your eye for that shape before scanning the outcrop.




