Sibirskite is a rare calcium borate mineral typically found in metamorphosed carbonate rocks associated with skarn deposits. It usually occurs as small, white to colorless platy or fibrous crystalline aggregates. It is primarily a collector's mineral known from the Tayozhnoye iron ore deposit in the Sakha Republic of Russia.

Hardness
3-4
Mohs
Luster
Vitreous
Streak
White
Transparency
Semitransparent

Is this sibirskite?

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 sibirskite with a known reference. Sibirskite sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: 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: colorless, dark gray.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: platy or fibrous aggregates.

Often confused with

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

Often found alongside sibirskite

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

All properties

Chemical formula
CaHBO₃
Mohs hardness
3-4
Density
2.58 g/cm³
Streak
White
Luster
Vitreous
Transparency
Semitransparent
Crystal system
Monoclinic
Crystal habit
Platy or fibrous aggregates
Cleavage
Good
Rarity
Rare
Uses
Collector, Research
Host rock
In veinlets and aggregates in skarns

Where rockhounds find sibirskite

Classic worldwide localities

  • Yuliya Svintsovaya Pb–Zn deposit, 20 km east-northeast of the Son railway station, Khakassia district, Siberia, Russia
  • Novofrolovskoye copper deposit, near Krasnoturinsk, Turinsk district, Northern Ural Mountains, Russia
  • Chersk and Selenyakhsk Ridges, Transbaikal, Russia
  • Fuka, near Bicchu, Okayama Prefecture, Japan

Field-hunting tip

Where it forms: In veinlets and aggregates in skarns. If you start seeing calcite, chlorite, pyrite in float, you are in the right ground. Typical habit: platy or fibrous aggregates. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify sibirskite?+
Mohs hardness is 3-4. Luster: vitreous. The streak is white. Common colors include colorless, dark gray.
Where is sibirskite found?+
Notable localities include Yuliya Svintsovaya Pb–Zn deposit, 20 km east-northeast of the Son railway station, Khakassia district, Siberia, Russia; Novofrolovskoye copper deposit, near Krasnoturinsk, Turinsk district, Northern Ural Mountains, Russia; Chersk and Selenyakhsk Ridges, Transbaikal, Russia; Fuka, near Bicchu, Okayama Prefecture, Japan.
What rocks look like sibirskite?+
Sibirskite is most often confused with Danburite, Colemanite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with sibirskite?+
Sibirskite commonly co-occurs with Calcite, Chlorite, Pyrite, Garnet, Vesuvianite, Datolite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does sibirskite form in?+
Where it forms: In veinlets and aggregates in skarns. Working float back to the host body is the standard way to chase a fresh occurrence.
What is sibirskite used for?+
Sibirskite is used in collector, research.

Find sibirskite on the map

RockHoundR shows mapped rockhounding spots, access rules, and lets you log every find.

Download on the App StoreGet it on Google Play