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 — that is 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.







