Edenite is a magnesium-rich member of the calcic amphibole group, typically occurring in metamorphosed carbonate rocks. It is most recognized for its short, prismatic to blocky crystal habit and distinct green or brownish coloring, and it is named after its type locality in Edenville, New York.
Is this edenite?
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 edenite with a known reference. Edenite sits at Mohs 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: bluish green, colorless, gray, white, light green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular.
Often confused with
Edenite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside edenite
Minerals reported to co-occur with edenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCa₂Mg₅(Si₇Al)O₂₂(OH)₂
- Mohs hardness
- 6
- Density
- 3.05-3.37 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular
- Cleavage
- Good on {110}, intersecting at 56° and 124°; partings on {100}, {001}
- Fluorescence
- Pale green-blue under SW UV
- Rarity
- Uncommon
- Uses
- Collector, Scientific research
- Host rock
- In intermediate plutonic igneous and medium-grade metamorphic rocks, as amphibolites and marbles
Where rockhounds find edenite
Classic worldwide localities
- Perhaps from Edenville, Orange Co., New York, and Franklin and Sterling Hill, Ogdensburg, Sussex Co., New Jersey, USA
- Tory Hill, near Bancroft, and at Wilberforce, Ontario, Canada
- Kotaki, Niigata Prefecture, Japan
Field-hunting tip
Where it forms: In intermediate plutonic igneous and medium-grade metamorphic rocks, as amphibolites and marbles. If you start seeing titanite, mica, chondrodite in float, you are in the right ground. Typical habit: tabular. Train your eye for that shape before scanning the outcrop.






