Lonecreekite is an extremely rare ammonium iron sulfate mineral that forms as small, colorless octahedrons. It is typically found as a secondary mineral in shale, resulting from the weathering of iron-rich sulfides, and is highly soluble in water, requiring dry storage for preservation.

Hardness
2-3
Mohs
Luster
Vitreous
Streak
White
Transparency
Transparent

Is this lonecreekite?

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 lonecreekite with a known reference. Lonecreekite sits at Mohs 2-3, 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.
  • 5
    Look at form & habit
    Crystal system: cubic. Typical habit: octahedral crystals.

Often confused with

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

Often found alongside lonecreekite

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

All properties

Chemical formula
(NH₄)Fe(SO₄)₂·12H₂O
Mohs hardness
2-3
Density
1.693 g/cm³
Colors
Streak
White
Luster
Vitreous
Transparency
Transparent
Crystal system
Cubic
Crystal habit
Octahedral crystals
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
A rare secondary mineral probably formed by alteration of pyrite and reaction, at pH < 1, with ammonia fumes produced as the result of decay of organic matter (Hyrax excreta)

Where rockhounds find lonecreekite

Classic worldwide localities

  • Lone Creek Fall cave, near Sabie, eastern Transvaal, South Africa (type locality)

Field-hunting tip

Where it forms: A rare secondary mineral probably formed by alteration of pyrite and reaction, at pH < 1, with ammonia fumes produced as the result of decay of organic matter (Hyrax excreta). If you start seeing clairite, sabieite, tschermigite in float, you are in the right ground. Typical habit: octahedral crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify lonecreekite?+
Mohs hardness is 2-3. Luster: vitreous. The streak is white. Common colors include colorless.
Where is lonecreekite found?+
Notable localities include Lone Creek Fall cave, near Sabie, eastern Transvaal, South Africa (type locality).
What rocks look like lonecreekite?+
Lonecreekite is most often confused with Tschermigite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with lonecreekite?+
Lonecreekite commonly co-occurs with Clairite, Sabieite, Tschermigite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does lonecreekite form in?+
Where it forms: A rare secondary mineral probably formed by alteration of pyrite and reaction, at pH < 1, with ammonia fumes produced as the result of decay of organic matter (Hyrax excreta). Working float back to the host body is the standard way to chase a fresh occurrence.
What is lonecreekite used for?+
Lonecreekite is used in collector.

Find lonecreekite on the map

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