Smaragdite is a chromium-rich, emerald-green variety of actinolite or hornblende commonly associated with corundum. It is most often found as a fine-grained, massive constituent within eclogite or metamorphic rocks, favored by lapidary artists for carving.
Is this smaragdite?
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 smaragdite with a known reference. Smaragdite sits at Mohs 5-6, 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.
- 4Match the color rangeCompare against the expected color range: emerald green, grass green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous.
Often confused with
Smaragdite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside smaragdite
Minerals reported to co-occur with smaragdite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂(Mg,Fe²⁺)₅Si₈O₂₂(OH)₂
- Mohs hardness
- 5-6
- Density
- 3.2-3.4 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous
- Cleavage
- Perfect in two directions
- Rarity
- Uncommon
- Uses
- Collector, Lapidary
- Host rock
- metamorphic
Where rockhounds find smaragdite
2 mapped spotsClassic worldwide localities
- Austria
- Italy
- North Carolina, USA
- Norway
Field-hunting tip
Where it forms: metamorphic. If you start seeing corundum, zoisite, plagioclase in float, you are in the right ground. Typical habit: fibrous. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in North Carolina. Start trip planning there.






