Pertsevite-(F) is a very rare magnesium borate mineral primarily found in high-temperature magnesium-rich skarn environments. It typically occurs as small prismatic crystals or irregular grains, often embedded within carbonate or silicate matrices. Collectors generally only encounter this mineral in specialized mineralogical collections due to its limited type locality in Russia.

Hardness
5-6
Mohs
Luster
Vitreous
Streak
Uneven
Transparency
Transparent

Is this pertsevite-(f)?

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 pertsevite-(f) with a known reference. Pertsevite-(F) sits at Mohs 5-6, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: uneven.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: brown, colorless, gray.
  • 5
    Look at form & habit
    Crystal system: orthorhombic. Typical habit: prismatic crystals, grains.

Often found alongside pertsevite-(f)

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

All properties

Chemical formula
Mg₂BO₃F
Mohs hardness
5-6
Density
3.12 g/cm³
Streak
Uneven
Luster
Vitreous
Transparency
Transparent
Crystal system
Orthorhombic
Crystal habit
Prismatic crystals, grains
Cleavage
None
Rarity
Rare
Uses
Collector, Scientific research
Host rock
In kotoite-marble skarn

Where rockhounds find pertsevite-(f)

Classic worldwide localities

  • Tas-Khayakhtakh ridge, Chersky Mountain System, near the mouth of Kebirin’ya Creek, a northern tributary of the Dogdo River, ~250 km east of Verkhoyansk, Republic of Sakha-Yakutia, Russia

Field-hunting tip

Where it forms: In kotoite-marble skarn. If you start seeing calcite, spinel, löllingite in float, you are in the right ground. Typical habit: prismatic crystals, grains. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify pertsevite-(f)?+
Mohs hardness is 5-6. Luster: vitreous. The streak is uneven. Common colors include brown, colorless, gray.
Where is pertsevite-(f) found?+
Notable localities include Tas-Khayakhtakh ridge, Chersky Mountain System, near the mouth of Kebirin’ya Creek, a northern tributary of the Dogdo River, ~250 km east of Verkhoyansk, Republic of Sakha-Yakutia, Russia.
What minerals are found with pertsevite-(f)?+
Pertsevite-(F) commonly co-occurs with Calcite, Spinel, Löllingite, Ludwigite, Aluminomagnesiohulsite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does pertsevite-(f) form in?+
Where it forms: In kotoite-marble skarn. Working float back to the host body is the standard way to chase a fresh occurrence.
What is pertsevite-(f) used for?+
Pertsevite-(F) is used in collector, scientific research.

Find pertsevite-(f) on the map

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