Humite is a rare member of the humite group typically found in contact metamorphosed carbonate rocks. It is most easily recognized by its distinct orange-yellow to brownish-red hues and vitreous luster in granular or crystalline aggregates.
Is this humite?
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 humite with a known reference. Humite 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. Humite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Humite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, orange, reddish-brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: granular, compact masses, or small rounded orthorhombic crystals.
Often confused with
Humite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside humite
Minerals reported to co-occur with humite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Mg,Fe)₇(SiO₄)₃(F,OH)₂
- Mohs hardness
- 6-6.5
- Density
- 3.1-3.2 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Granular, Compact Masses, Or Small Rounded Orthorhombic Crystals
- Cleavage
- Poor On {001}
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Metamorphosed Limestones and Dolomites
- Typical price
- $10-100 per specimen
Where rockhounds find humite
Classic worldwide localities
- Monte Somma, Italy
- Amity, New York, USA
- Pargas, Finland
- Kukh-i-Lal, Tajikistan
- Norberg, Sweden
Field-hunting tip
Look in metamorphosed limestones and dolomites country, the host setting where humite typically forms. If you start seeing calcite, dolomite, spinels in float, you are in the right ground. Field specimens usually show a granular, compact masses, or small rounded orthorhombic crystals habit, so train your eye for that shape before scanning the outcrop.






