Retzian-(La) is an extremely rare arsenate mineral member of the retzian group. It is primarily found in the metamorphosed manganese mines of Sweden as small, reddish-brown crystals, and it requires advanced analytical methods for positive identification due to its similarity to other members of the group.
Is this retzian-(la)?
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-(la) with a known reference. Retzian-(La) 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: pale brown.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous on {010} and fractures, otherwise dull.
- 4Match the color rangeCompare against the expected color range: reddish brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, granular masses.
Often confused with
Retzian-(La) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside retzian-(la)
Minerals reported to co-occur with retzian-(la). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn₂LaAsO₄(OH)₄
- Mohs hardness
- 3-4
- Density
- 4.49 g/cm³
- Colors
- Streak
- Pale brown
- Luster
- Vitreous on {010} and fractures, otherwise dull
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular crystals, granular masses
- 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-(la)
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 willemite, franklinite, calcite in float, you are in the right ground. Typical habit: tabular crystals, granular masses. Train your eye for that shape before scanning the outcrop.





