Pittongite is a rare sodium tungsten iron hydroxide, typically cream yellow. It was approved as a distinct mineral species in 2005. It was first described from mine dumps near the main shaft of a tungsten deposit (Bass and Watson's) 6 km west of Linton (near Ballarat), New England District, Victoria, Australia.

Hardness
2-3
Mohs
Luster
Pearly to earthy
Streak
Cream
Transparency
Transparent

Is this pittongite?

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 pittongite with a known reference. Pittongite 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: cream.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: pearly to earthy.
  • 4
    Match the color range
    Compare against the expected color range: creamy yellow.
  • 5
    Look at form & habit
    Crystal system: hexagonal. Typical habit: aggregates.

Often confused with

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

Often found alongside pittongite

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

All properties

Chemical formula
(Na,H₂O)₀.₇(W,Fe³⁺)(O,OH)₃
Mohs hardness
2-3
Density
5.715 g/cm³
Colors
Creamy yellow
Streak
Cream
Luster
Pearly to earthy
Transparency
Transparent
Crystal system
Hexagonal
Crystal habit
Aggregates
Cleavage
None observed
Rarity
Rare
Uses
Collector
Host rock
Formed by weathering ferberite in hydrothermal quartz veins associated with granite by chemical reaction with acidic, oxidizing solutions containing sodium

Where rockhounds find pittongite

Classic worldwide localities

  • Mine dumps near the main shaft of a tungsten deposit 35 km west of Ballerat in the New England District of New South Wales, Australia (type locality)

Field-hunting tip

Where it forms: Formed by weathering ferberite in hydrothermal quartz veins associated with granite by chemical reaction with acidic, oxidizing solutions containing sodium. If you start seeing ferberite, quartz, bismuth in float, you are in the right ground. Typical habit: aggregates. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify pittongite?+
Mohs hardness is 2-3. Luster: pearly to earthy. The streak is cream. Common colors include creamy yellow.
Where is pittongite found?+
Notable localities include Mine dumps near the main shaft of a tungsten deposit 35 km west of Ballerat in the New England District of New South Wales, Australia (type locality).
What rocks look like pittongite?+
Pittongite is most often confused with Bindheimite, Stibiconite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with pittongite?+
Pittongite commonly co-occurs with Ferberite, Quartz, Bismuth, Gold, Bismuthinite, Koechlinite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does pittongite form in?+
Where it forms: Formed by weathering ferberite in hydrothermal quartz veins associated with granite by chemical reaction with acidic, oxidizing solutions containing sodium. Working float back to the host body is the standard way to chase a fresh occurrence.
What is pittongite used for?+
Pittongite is used in collector.

Find pittongite on the map

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