Oxy-schorl is a relatively recently defined mineral species within the tourmaline supergroup, specifically recognized as the oxy-analogue of schorl. It typically appears as black, prismatic crystals that are macroscopically indistinguishable from common schorl without advanced analytical techniques. Collectors generally identify it by its specific geochemical context in evolved pegmatites and granitic environments.

Hardness
7
Mohs
Luster
Vitreous
Streak
Pale Gray
Transparency
Translucent

Is this oxy-schorl?

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 oxy-schorl with a known reference. Oxy-schorl sits at Mohs 7, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Oxy-schorl leaves a pale gray streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Oxy-schorl typically shows a vitreous luster.
  • 4
    Match the color range
    Compare against the expected color range: black, brownish-black.
  • 5
    Look at form & habit
    Crystal system: trigonal. Typical habit: prismatic crystals with rounded triangular cross-sections, often striated.

Often confused with

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

Often found alongside oxy-schorl

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

All properties

Chemical formula
Na(Fe²⁺₂Al)Al₆Si₆O₁₈(BO₃)₃(OH)₃O
Mohs hardness
7
Density
3.18-3.25 g/cm³
Streak
Pale Gray
Luster
Vitreous
Transparency
Translucent
Crystal system
Trigonal
Crystal habit
Prismatic Crystals with Rounded Triangular Cross-sections, Often Striated
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
Granite Pegmatites

Where rockhounds find oxy-schorl

Classic worldwide localities

  • Czech Republic
  • Germany
  • Italy
  • Norway

Field-hunting tip

Look in granite pegmatites country, the host setting where oxy-schorl typically forms. If you start seeing quartz, albite, microcline in float, you are in the right ground. Field specimens usually show a prismatic crystals with rounded triangular cross-sections, often striated habit, so train your eye for that shape before scanning the outcrop.

Common questions

How do you identify oxy-schorl?+
Mohs hardness is 7. It typically shows a vitreous luster. The streak is pale gray. Common colors include black, brownish-black.
Where is oxy-schorl found?+
Notable localities include Czech Republic; Germany; Italy; Norway.
What rocks look like oxy-schorl?+
Oxy-schorl is most often confused with Schorl, Dravite, Foitite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with oxy-schorl?+
Oxy-schorl commonly co-occurs with Quartz, Albite, Microcline, Muscovite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does oxy-schorl form in?+
Oxy-schorl typically forms in granite pegmatites. Working float back to the host body is the standard way to chase a fresh occurrence.
What is oxy-schorl used for?+
Oxy-schorl is used in collector.

Find oxy-schorl on the map

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