Efremovite is a rare sulfate mineral that typically forms as a result of spontaneous combustion in coal mine dumps. It is structurally part of the langbeinite group and is primarily found as small, yellowish or colorless crystals associated with other minerals formed by fumarolic or pyrometamorphic processes in burning coal seams.

Hardness
~2
Mohs
Luster
Vitreous
Streak
White
Transparency
Transparent to nearly opaque

Is this efremovite?

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 efremovite with a known reference. Efremovite sits at Mohs ~2, 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: gray white, white.
  • 5
    Look at form & habit
    Crystal system: cubic. Typical habit: equant crystals, granular.

Often confused with

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

Often found alongside efremovite

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

All properties

Chemical formula
(NH₄)₂Mg₂(SO₄)₃
Mohs hardness
~2
Density
2.52 g/cm³
Streak
White
Luster
Vitreous
Transparency
Transparent to nearly opaque
Crystal system
Cubic
Crystal habit
Equant crystals, granular
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
As crusts on burning coal mine dumps, formed by the reaction of combustion gases with carbonate rocks

Where rockhounds find efremovite

Classic worldwide localities

  • Kopeysk, in the Chelyabinsk coal basin, Southern Ural Mountains, Russia
  • Scholler mine, near Kladno, Czech Republic

Field-hunting tip

Where it forms: As crusts on burning coal mine dumps, formed by the reaction of combustion gases with carbonate rocks. If you start seeing sulfur, kladnoite, mascagnite in float, you are in the right ground. Typical habit: equant crystals, granular. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify efremovite?+
Mohs hardness is ~2. Luster: vitreous. The streak is white. Common colors include gray white, white.
Where is efremovite found?+
Notable localities include Kopeysk, in the Chelyabinsk coal basin, Southern Ural Mountains, Russia; Scholler mine, near Kladno, Czech Republic.
What rocks look like efremovite?+
Efremovite is most often confused with Langbeinite, Manganolangbeinite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with efremovite?+
Efremovite commonly co-occurs with Sulfur, Kladnoite, Mascagnite, Boussingaultite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does efremovite form in?+
Where it forms: As crusts on burning coal mine dumps, formed by the reaction of combustion gases with carbonate rocks. Working float back to the host body is the standard way to chase a fresh occurrence.
What is efremovite used for?+
Efremovite is used in collector.

Find efremovite on the map

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