Steklite is an extremely rare potassium aluminum sulfate mineral found primarily in fumarolic deposits. It is known to occur as thin, transparent, tabular crystals associated with other secondary sulfate minerals at active volcanic sites.

Hardness
2.5
Mohs
Luster
Vitreous
Streak
White
Transparency
Transparent

Is this steklite?

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 steklite with a known reference. Steklite sits at Mohs 2.5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: 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, white, grayish-white in aggregates.
  • 5
    Look at form & habit
    Crystal system: trigonal. Typical habit: tabular crystals.

Often confused with

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

Often found alongside steklite

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

All properties

Chemical formula
KAl(SO₄)₂
Mohs hardness
2.5
Density
2.797 g/cm³
Colors
ColorlessWhiteGrayish-white in aggregates
Streak
White
Luster
Vitreous
Transparency
Transparent
Crystal system
Trigonal
Crystal habit
Tabular crystals
Cleavage
Perfect on {001}
Rarity
Rare
Uses
Collector
Host rock
A volcanic sublimate formed at 150-170 °C as part of sulfate crusts around an active fumarole

Where rockhounds find steklite

Classic worldwide localities

  • Burning anthracite coal deposits Eastern Pennsylvania, USA
  • Second scoria cone of the Northern Breakthrough of the Great Tolbachik Fissure Eruption (1975–1976), Tolbachik volcano, Kamchatka, and the dumps of coal mine N 47 near Kopeisk, South Urals, Russia
  • Showashinzan volcano, Hokkaido, Japan
  • Izalco volcano, El Salvador and Santiaguit volcano, Guatemala

Field-hunting tip

Where it forms: A volcanic sublimate formed at 150-170 °C as part of sulfate crusts around an active fumarole. If you start seeing alumoklyuchevskite, langbeinite, euchlorine in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify steklite?+
Mohs hardness is 2.5. Luster: vitreous. The streak is white. Common colors include colorless, white, grayish-white in aggregates.
Where is steklite found?+
Notable localities include Burning anthracite coal deposits Eastern Pennsylvania, USA; Second scoria cone of the Northern Breakthrough of the Great Tolbachik Fissure Eruption (1975–1976), Tolbachik volcano, Kamchatka, and the dumps of coal mine N 47 near Kopeisk, South Urals, Russia; Showashinzan volcano, Hokkaido, Japan; Izalco volcano, El Salvador and Santiaguit volcano, Guatemala.
What rocks look like steklite?+
Steklite is most often confused with Alunite, Millosevichite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with steklite?+
Steklite commonly co-occurs with Alumoklyuchevskite, Langbeinite, Euchlorine, Fedotovite, Chalcocyanite, Hematite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does steklite form in?+
Where it forms: A volcanic sublimate formed at 150-170 °C as part of sulfate crusts around an active fumarole. Working float back to the host body is the standard way to chase a fresh occurrence.
What is steklite used for?+
Steklite is used in collector.

Find steklite on the map

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