Rengeite is a rare strontium-zirconium sorosilicate mineral typically found in metamorphic rocks. Collectors prize it for its association with unique geological occurrences in Japan where it forms tabular, dark-colored crystals.
Is this rengeite?
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 rengeite with a known reference. Rengeite 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: pale greenish brown.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine.
- 4Match the color rangeCompare against the expected color range: dark greenish brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: anhedral grains, microscopic crystals.
Often confused with
Rengeite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside rengeite
Minerals reported to co-occur with rengeite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Sr₄ZrTi₄Si₄O₂₂
- Mohs hardness
- 5-5.5
- Density
- 4.12 g/cm³
- Colors
- Dark greenish brown
- Streak
- Pale greenish brown
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Anhedral grains, microscopic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In jade pebbles from rocks in a high P/T metamorphic belt as tectonic inclusions in serpentinite melange
Where rockhounds find rengeite
Classic worldwide localities
- Oyashirazu shore, Sea of Japan, Ohmi Town
- Beds of the Kotakigawa and Himekawa rivers, Itoigawa City, Ohmi region, Niigata Prefecture, Japan
Field-hunting tip
Where it forms: In jade pebbles from rocks in a high P/T metamorphic belt as tectonic inclusions in serpentinite melange. If you start seeing jadeite, natrolite, rutile in float, you are in the right ground. Typical habit: anhedral grains, microscopic crystals. Train your eye for that shape before scanning the outcrop.






