Studenitsite is a rare borate mineral that occurs as small, clear to white prismatic crystals. It is primarily found within evaporite-related sedimentary environments, most notably in its type locality in North Macedonia. Collectors prize it for its rarity and its role as a specialized member of the borate mineral group.

Hardness
5.5-6
Mohs
Luster
Vitreous
Streak
White
Transparency
Translucent to transparent in thin pieces

Is this studenitsite?

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 studenitsite with a known reference. Studenitsite sits at Mohs 5.5-6, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: 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, light dirty yellow, light gray.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: striated, wedge shaped.

Often confused with

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

Often found alongside studenitsite

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

All properties

Chemical formula
NaCa₂B₉O₁₄(OH)₄·2H₂O
Mohs hardness
5.5-6
Density
2.29 g/cm³
Colors
ColorlessLight dirty yellowLight gray
Streak
White
Luster
Vitreous
Transparency
Translucent to transparent in thin pieces
Crystal system
Monoclinic
Crystal habit
Striated, wedge shaped
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
As lenses in clay and carbonate-bearing volcanogenic-sedimentary borate deposits

Where rockhounds find studenitsite

Classic worldwide localities

  • Piskaya deposit, Yarondolskii Basin, on the Ibar River, 280 km south of Belgrade, Yugoslavia

Field-hunting tip

Where it forms: As lenses in clay and carbonate-bearing volcanogenic-sedimentary borate deposits. If you start seeing colemanite, howlite, ulexite in float, you are in the right ground. Typical habit: striated, wedge shaped. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify studenitsite?+
Mohs hardness is 5.5-6. Luster: vitreous. The streak is white. Common colors include colorless, light dirty yellow, light gray.
Where is studenitsite found?+
Notable localities include Piskaya deposit, Yarondolskii Basin, on the Ibar River, 280 km south of Belgrade, Yugoslavia.
What rocks look like studenitsite?+
Studenitsite is most often confused with Ulexite, Colemanite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with studenitsite?+
Studenitsite commonly co-occurs with Colemanite, Howlite, Ulexite, Pentahydroborite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does studenitsite form in?+
Where it forms: As lenses in clay and carbonate-bearing volcanogenic-sedimentary borate deposits. Working float back to the host body is the standard way to chase a fresh occurrence.
What is studenitsite used for?+
Studenitsite is used in collector.

Find studenitsite on the map

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