Høgtuvaite is a rare member of the aenigmatite group found primarily in alkaline syenite pegmatites in Norway. It typically appears as dark, tabular crystals and is distinguished from its group relatives by its specific chemical composition and complex crystal structure.

Hardness
5.5
Mohs
Luster
Subadamantine to nonmetallic
Streak
Dark green
Transparency
Translucent

Is this høgtuvaite?

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 høgtuvaite with a known reference. Høgtuvaite sits at Mohs 5.5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: dark green.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: subadamantine to nonmetallic.
  • 4
    Match the color range
    Compare against the expected color range: black.
  • 5
    Look at form & habit
    Crystal system: triclinic. Typical habit: tabular crystals.

Often confused with

Høgtuvaite vs. its common look-alikes, and how to tell them apart in the field.

Often found alongside høgtuvaite

Minerals reported to co-occur with høgtuvaite. Spotting these in float or country rock is a strong cue you are in the right ground.

All properties

Chemical formula
Ca₄(Fe₆Fe₆)O₄[Si₈Be₂Al₂O₃₆]
Mohs hardness
5.5
Density
3.85-3.88 g/cm³
Colors
Streak
Dark green
Luster
Subadamantine to nonmetallic
Transparency
Translucent
Crystal system
Triclinic
Crystal habit
Tabular crystals
Rarity
Rare
Uses
Collector
Host rock
As a late-stage metamorphic mineral in peraluminous granitic gneisses and mafic pegmatites associated with a beryllium deposit (near Mo i Rana, Norway)

Where rockhounds find høgtuvaite

Classic worldwide localities

  • Found about 16 km northwest of Mo i Rana, Norway
  • Ilmen Mountains, Southern Ural Mountains, Russia

Field-hunting tip

Where it forms: As a late-stage metamorphic mineral in peraluminous granitic gneisses and mafic pegmatites associated with a beryllium deposit (near Mo i Rana, Norway). If you start seeing quartz, albite, microcline in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify høgtuvaite?+
Mohs hardness is 5.5. Luster: subadamantine to nonmetallic. The streak is dark green. Common colors include black.
Where is høgtuvaite found?+
Notable localities include Found about 16 km northwest of Mo i Rana, Norway; Ilmen Mountains, Southern Ural Mountains, Russia.
Is høgtuvaite safe to handle?+
Høgtuvaite contains beryllium. Wash your hands afterwards, never grind or breathe the dust, and store it apart from specimens you handle often.
What rocks look like høgtuvaite?+
Høgtuvaite is most often confused with Aenigmatite, Rhönite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with høgtuvaite?+
Høgtuvaite commonly co-occurs with Quartz, Albite, Microcline, Biotite, Phenakite, Zircon. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does høgtuvaite form in?+
Where it forms: As a late-stage metamorphic mineral in peraluminous granitic gneisses and mafic pegmatites associated with a beryllium deposit (near Mo i Rana, Norway). Working float back to the host body is the standard way to chase a fresh occurrence.
What is høgtuvaite used for?+
Høgtuvaite is used in collector.

Find høgtuvaite on the map

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