Peterandresenite is a rare manganese niobium oxide, typically orange. It was approved as a distinct mineral species in 2012. It was first described from AS Granit larvikite, Tvedalen, Larvik, Vestfold, Norway.
Is this peterandresenite?
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 peterandresenite with a known reference. Peterandresenite sits at Mohs 2-2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale orange.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to resinous.
- 4Match the color rangeCompare against the expected color range: orange.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals.
Often confused with
Peterandresenite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside peterandresenite
Minerals reported to co-occur with peterandresenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn₄Nb₆O₁₉(H₂O)₁₂·2H₂O
- Mohs hardness
- 2-2.5
- Density
- 3.10 g/cm³
- Colors
- Streak
- Pale orange
- Luster
- Vitreous to resinous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Formed at the hydrothermal stage on fracture surfaces and in tiny vugs in the center of a miaskitic pegmatite dike within the larvikites of a plutonic complex
Where rockhounds find peterandresenite
Classic worldwide localities
- Granit larvikite (quarry level 4), Tvedalen, Larvik, Vestfold, Norway
Field-hunting tip
Where it forms: Formed at the hydrothermal stage on fracture surfaces and in tiny vugs in the center of a miaskitic pegmatite dike within the larvikites of a plutonic complex. If you start seeing analcime, fluorapophyllite-, arsenopyrite in float, you are in the right ground. Typical habit: platy crystals. Train your eye for that shape before scanning the outcrop.







