Clinokurchatovite is a rare borate mineral found predominantly in magnesian skarn deposits. It is chemically similar to Kurchatovite but structurally distinct due to its monoclinic-like tendencies in complex borate groupings. Collectors typically find it as inconspicuous granular masses associated with other borates and magnetite.

Hardness
4.5
Mohs
Luster
Vitreous
Streak
Gray white
Transparency
Semitransparent

Is this clinokurchatovite?

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 clinokurchatovite with a known reference. Clinokurchatovite sits at Mohs 4.5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: gray white.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: light gray.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: granular aggregates, massive.

Often confused with

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

Often found alongside clinokurchatovite

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

All properties

Chemical formula
CaMgB₂O₅
Mohs hardness
4.5
Density
3.07-3.08 g/cm³
Streak
Gray white
Luster
Vitreous
Transparency
Semitransparent
Crystal system
Monoclinic
Crystal habit
Granular aggregates, massive
Cleavage
Distinct
Rarity
Rare
Uses
Collector
Host rock
A replacement of kurchatovite in boron-bearing rocks

Where rockhounds find clinokurchatovite

Classic worldwide localities

  • Sayak-IV boron deposit, northeast Balkhash region, Kazakhstan
  • Solongo boron deposit, Buryatia, Russia
  • Titovskoye boron deposit, Tas-Khayakhtakh Mountains, Sakha, Russia
  • Novofrolovskoye copper deposit, near Krasnoturinsk, Turinsk district, Northern Ural Mountains, Russia

Field-hunting tip

Where it forms: A replacement of kurchatovite in boron-bearing rocks. If you start seeing kurchatovite, suanite, ludwigite in float, you are in the right ground. Typical habit: granular aggregates, massive. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify clinokurchatovite?+
Mohs hardness is 4.5. Luster: vitreous. The streak is gray white. Common colors include light gray.
Where is clinokurchatovite found?+
Notable localities include Sayak-IV boron deposit, northeast Balkhash region, Kazakhstan; Solongo boron deposit, Buryatia, Russia; Titovskoye boron deposit, Tas-Khayakhtakh Mountains, Sakha, Russia; Novofrolovskoye copper deposit, near Krasnoturinsk, Turinsk district, Northern Ural Mountains, Russia.
What rocks look like clinokurchatovite?+
Clinokurchatovite is most often confused with Kurchatovite, Suanite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with clinokurchatovite?+
Clinokurchatovite commonly co-occurs with Kurchatovite, Suanite, Ludwigite, Szaibélyite, Sakhaite, Clinohumite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does clinokurchatovite form in?+
Where it forms: A replacement of kurchatovite in boron-bearing rocks. Working float back to the host body is the standard way to chase a fresh occurrence.
What is clinokurchatovite used for?+
Clinokurchatovite is used in collector.

Find clinokurchatovite on the map

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