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.

Hardness
2-2.5
Mohs
Luster
Vitreous to resinous
Streak
Pale orange
Transparency
Transparent to translucent

Is this peterandresenite?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try 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.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: pale orange.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous to resinous.
  • 4
    Match the color range
    Compare against the expected color range: orange.
  • 5
    Look at form & habit
    Crystal 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.

Common questions

How do you identify peterandresenite?+
Mohs hardness is 2-2.5. Luster: vitreous to resinous. The streak is pale orange. Common colors include orange.
Where is peterandresenite found?+
Notable localities include Granit larvikite (quarry level 4), Tvedalen, Larvik, Vestfold, Norway.
What rocks look like peterandresenite?+
Peterandresenite is most often confused with Manganberzeliite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with peterandresenite?+
Peterandresenite commonly co-occurs with Analcime, Fluorapophyllite-, Arsenopyrite, Behoite, Bertrandite, Calcite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does peterandresenite form in?+
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. Working float back to the host body is the standard way to chase a fresh occurrence.
What is peterandresenite used for?+
Peterandresenite is used in collector.

Find peterandresenite on the map

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