Monticellite is an uncommon calcium-magnesium silicate belonging to the olivine group. It typically occurs as small, pale prismatic crystals or granular aggregates in contact-metamorphosed limestone and is most often identified by its association with skarn minerals.
Is this monticellite?
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 monticellite with a known reference. Monticellite sits at Mohs 5-5.5, 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: vitreous, slightly resinous when massive.
- 4Match the color rangeCompare against the expected color range: colorless, greenish gray, gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: crystalline, prismatic.
Often confused with
Monticellite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside monticellite
Minerals reported to co-occur with monticellite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaMgSiO₄
- Mohs hardness
- 5-5.5
- Density
- 3.03-3.27 g/cm³
- Streak
- White
- Luster
- Vitreous, slightly resinous when massive
- Transparency
- Transparent to translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Crystalline, prismatic
- Cleavage
- Poor on {010}
- Rarity
- Uncommon
- Uses
- Collector, Scientific research
- Host rock
- Formed during metamorphism of siliceous dolostones; in contact metamorphic deposits between limestones and olivine gabbros; in skarns at granite-dolomitic limestone contacts; rarely in kimberlites
Where rockhounds find monticellite
1 mapped spotsClassic worldwide localities
- Crestmore, Riverside Co., California, USA
- Cascade Mountain, Essex Co., New York, USA
- Magnet Cove, Hot Spring Co., Arkansas, USA
- Monte Somma and Vesuvius, Campania, Italy
- Scawt Hill, near Larne, Co. Antrim, Ireland
- Isle Cadieux and Oka, Quebec, Canada
Field-hunting tip
Where it forms: Formed during metamorphism of siliceous dolostones; in contact metamorphic deposits between limestones and olivine gabbros; in skarns at granite-dolomitic limestone contacts; rarely in kimberlites. If you start seeing gehlenite, spinel, calcite in float, you are in the right ground. Typical habit: crystalline, prismatic. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Arkansas. Start trip planning there.









