Retzian-(Nd) is an extremely rare manganese arsenate mineral belonging to the Retzian group. It typically occurs as small, brownish tabular crystals in metamorphosed manganese deposits, most notably the famous Långban mines in Sweden.
Is this retzian-(nd)?
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 retzian-(nd) with a known reference. Retzian-(Nd) sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: very pale brown.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to dull.
- 4Match the color rangeCompare against the expected color range: pink brown, reddish brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, granular.
Often confused with
Retzian-(Nd) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside retzian-(nd)
Minerals reported to co-occur with retzian-(nd). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn₂Nd(AsO₄)(OH)₄
- Mohs hardness
- 3-4
- Density
- 4.45 g/cm³
- Colors
- Streak
- Very pale brown
- Luster
- Vitreous to dull
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular crystals, granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A very rare late phase in fractures in a metamorphosed stratiform zinc orebody
Where rockhounds find retzian-(nd)
Classic worldwide localities
- Sterling Hill, Ogdensburg, Sussex Co., New Jersey, USA
Field-hunting tip
Where it forms: A very rare late phase in fractures in a metamorphosed stratiform zinc orebody. If you start seeing rhodochrosite, kraisslite, sonolite in float, you are in the right ground. Typical habit: tabular crystals, granular. Train your eye for that shape before scanning the outcrop.






