Quenstedtite is a rare hydrated iron sulfate mineral typically found as a secondary product in the oxidized zones of ore deposits. It is known for its distinct pale violet color, though it is highly soluble and must be kept away from humidity to prevent dehydration or degradation.

Hardness
2.5
Mohs
Luster
Vitreous
Streak
Light violet blue
Transparency
Transparent

Is this quenstedtite?

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 quenstedtite with a known reference. Quenstedtite 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: light violet blue.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: white, light violet, red violet.
  • 5
    Look at form & habit
    Crystal system: triclinic. Typical habit: euhedral crystals, granular.

Often confused with

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

Often found alongside quenstedtite

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

All properties

Chemical formula
Fe₂(SO₄)₃·11H₂O
Mohs hardness
2.5
Density
2.11-2.15 g/cm³
Colors
Streak
Light violet blue
Luster
Vitreous
Transparency
Transparent
Crystal system
Triclinic
Crystal habit
Euhedral crystals, granular
Cleavage
Perfect on {010}; good on {100}
Rarity
Rare
Uses
Collector
Host rock
An uncommon mineral formed in the oxidized zone of pyrite-rich mineral deposits especially in arid regions

Where rockhounds find quenstedtite

Classic worldwide localities

  • Sulphur Hole prospect, near Borate, about 10 km northeast of Yermo, Calico Mountains, San Bernardino Co., California, USA
  • Tierra Amarilla, southeast of Copiapó, Atacama, and at Alcaparrosa, near Cerritos Bayos, southwest of Calama, Antofagasta, Chile
  • Baňská Štiavnica (Schemnitz), Slovakia
  • Richelsdorfer Mountains, Hesse, Germany
  • Dyakhtardakh cassiterite–sulfide deposit, northeastern Sakha, Russia

Field-hunting tip

Where it forms: An uncommon mineral formed in the oxidized zone of pyrite-rich mineral deposits especially in arid regions. If you start seeing coquimbite, copiapite, römerite in float, you are in the right ground. Typical habit: euhedral crystals, granular. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify quenstedtite?+
Mohs hardness is 2.5. Luster: vitreous. The streak is light violet blue. Common colors include white, light violet, red violet.
Where is quenstedtite found?+
Notable localities include Sulphur Hole prospect, near Borate, about 10 km northeast of Yermo, Calico Mountains, San Bernardino Co., California, USA; Tierra Amarilla, southeast of Copiapó, Atacama, and at Alcaparrosa, near Cerritos Bayos, southwest of Calama, Antofagasta, Chile; Baňská Štiavnica (Schemnitz), Slovakia; Richelsdorfer Mountains, Hesse, Germany; Dyakhtardakh cassiterite–sulfide deposit, northeastern Sakha, Russia.
What rocks look like quenstedtite?+
Quenstedtite is most often confused with Copiapite, Coquimbite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with quenstedtite?+
Quenstedtite commonly co-occurs with Coquimbite, Copiapite, Römerite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does quenstedtite form in?+
Where it forms: An uncommon mineral formed in the oxidized zone of pyrite-rich mineral deposits especially in arid regions. Working float back to the host body is the standard way to chase a fresh occurrence.
What is quenstedtite used for?+
Quenstedtite is used in collector.

Find quenstedtite on the map

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