Hydrotungstite is a rare secondary tungsten mineral that typically forms as a result of the alteration of scheelite or other tungsten minerals. It is most commonly identified by its soft, yellow-to-green platy crystals that resemble mica, often found as crusts in weathered hydrothermal veins.

Hardness
2
Mohs
Luster
Vitreous to dull
Streak
Greenish yellow
Transparency
Semitransparent

Is this hydrotungstite?

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 hydrotungstite with a known reference. Hydrotungstite 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: greenish yellow.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous to dull.
  • 4
    Match the color range
    Compare against the expected color range: yellow green, dark green.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: platy or micaceous aggregates, crusts.

Often confused with

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

Often found alongside hydrotungstite

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

All properties

Chemical formula
WO₃·2H₂O
Mohs hardness
2
Density
4.60 g/cm³
Streak
Greenish yellow
Luster
Vitreous to dull
Transparency
Semitransparent
Crystal system
Monoclinic
Crystal habit
Platy or micaceous aggregates, crusts
Cleavage
{010}, imperfect
Rarity
Rare
Uses
Collector
Host rock
An alteration product of ferberite in the oxidized zone of a hydrothermal tungsten deposit, where it was an ore mineral (Calacalani mine, Bolivia)

Where rockhounds find hydrotungstite

Classic worldwide localities

  • Oruro district, at the San Antonio de Calacalani mine, near Colquiri, and in the Juliani mine, Bolivia
  • Panasqueira, Portugal
  • Grancarica scheelite deposit, southwest of Velingrad, Bulgaria

Field-hunting tip

Where it forms: An alteration product of ferberite in the oxidized zone of a hydrothermal tungsten deposit, where it was an ore mineral (Calacalani mine, Bolivia). If you start seeing ferberite, tungstite in float, you are in the right ground. Typical habit: platy or micaceous aggregates, crusts. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify hydrotungstite?+
Mohs hardness is 2. Luster: vitreous to dull. The streak is greenish yellow. Common colors include yellow green, dark green.
Where is hydrotungstite found?+
Notable localities include Oruro district, at the San Antonio de Calacalani mine, near Colquiri, and in the Juliani mine, Bolivia; Panasqueira, Portugal; Grancarica scheelite deposit, southwest of Velingrad, Bulgaria.
What rocks look like hydrotungstite?+
Hydrotungstite is most often confused with Tungstite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with hydrotungstite?+
Hydrotungstite commonly co-occurs with Ferberite, Tungstite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does hydrotungstite form in?+
Where it forms: An alteration product of ferberite in the oxidized zone of a hydrothermal tungsten deposit, where it was an ore mineral (Calacalani mine, Bolivia). Working float back to the host body is the standard way to chase a fresh occurrence.
What is hydrotungstite used for?+
Hydrotungstite is used in collector.

Find hydrotungstite on the map

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