Chondrodite is a member of the Humite group, frequently occurring as yellow to orange grains or small crystals embedded in contact-metamorphosed limestones. Collectors prize it for its strong fluorescence and distinct color, often seeking specimens from classic localities like the Franklin mining district.
Is this chondrodite?
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 chondrodite with a known reference. Chondrodite sits at Mohs 6-6.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: gray.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to resinous.
- 4Match the color rangeCompare against the expected color range: yellow, orange, brownish white, reddish white, greenish white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: crystalline, massive.
Often confused with
Chondrodite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Chondrodite leaves gray, Spessartine leaves white.

How to tell apart: Zircon is the harder of the two (Mohs 7.5 vs. 6-6.5); streak differs, so Chondrodite leaves gray, Zircon leaves white.

How to tell apart: Streak differs, so Chondrodite leaves gray, Clinohumite leaves white.
Often found alongside chondrodite
Minerals reported to co-occur with chondrodite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₅(SiO₄)₂F₂
- Mohs hardness
- 6-6.5
- Density
- 3.16-3.26 g/cm³
- Streak
- Gray
- Luster
- Vitreous to resinous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Crystalline, massive
- Cleavage
- {100} indistinct; parting on {001}
- Fluorescence
- Orange yellow under SW UV; orange under LW UV
- Rarity
- Uncommon
- Uses
- Collector, Gemstone
- Host rock
- In contact metamorphic zones, in limestones and dolostones, associated with felsic to alkalic plutonic rocks, especially with Fe-B-F metasomatism; in a carbonatite
Where rockhounds find chondrodite
3 mapped spotsClassic worldwide localities
- Tilly Foster mine, Brewster, Putnam Co., and Amity, Orange Co., New York, USA
- Franklin and Sparta, Sussex Co., New Jersey, USA
- Johnson Camp, Cochise Co., and the Lakeshore mine, Pinal Co., Arizona, USA
- Crestmore, Riverside Co., California, USA
- Pargas, Hangelby, and Sibbo, Finland
- Kafveltorp, near Kopparberg, Sweden
Field-hunting tip
Where it forms: In contact metamorphic zones, in limestones and dolostones, associated with felsic to alkalic plutonic rocks, especially with Fe-B-F metasomatism; in a carbonatite. If you start seeing phlogopite, spinel, magnetite in float, you are in the right ground. Typical habit: crystalline, massive. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in New Jersey, New York. Start trip planning there.






