Molybdite typically occurs as a bright yellow, fibrous, or earthy secondary mineral resulting from the oxidation of molybdenite. It is most commonly found as soft, delicate crusts or tufts in the weathered zones of molybdenum-rich ore deposits.

Hardness
3-4
Mohs
Luster
Adamantine
Streak
White
Transparency
Transparent

Is this molybdite?

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 molybdite with a known reference. Molybdite sits at Mohs 3-4, 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: adamantine.
  • 4
    Match the color range
    Compare against the expected color range: colorless, greenish yellow, light greenish yellow.
  • 5
    Look at form & habit
    Crystal system: orthorhombic. Typical habit: fibrous, earthy, pulverulent, or as crusts.

Often confused with

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

Often found alongside molybdite

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

All properties

Chemical formula
MoO₃
Mohs hardness
3-4
Density
4.72 g/cm³
Colors
ColorlessGreenish yellowLight greenish yellow
Streak
White
Luster
Adamantine
Transparency
Transparent
Crystal system
Orthorhombic
Crystal habit
Fibrous, earthy, pulverulent, or as crusts
Cleavage
{100}, perfect; {001}, distinct
Rarity
Uncommon
Uses
Collector
Host rock
In cavities and coating molybdenite in a weathered quartz vein near its contact with topaz-quartz greisen

Where rockhounds find molybdite

Classic worldwide localities

  • Krupka, Krušné hory Mountains, Czech Republic

Field-hunting tip

Where it forms: In cavities and coating molybdenite in a weathered quartz vein near its contact with topaz-quartz greisen. If you start seeing molybdenite, betpakdalite, quartz in float, you are in the right ground. Typical habit: fibrous, earthy, pulverulent, or as crusts. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify molybdite?+
Mohs hardness is 3-4. Luster: adamantine. The streak is white. Common colors include colorless, greenish yellow, light greenish yellow.
Where is molybdite found?+
Notable localities include Krupka, Krušné hory Mountains, Czech Republic.
What rocks look like molybdite?+
Molybdite is most often confused with Sulfur, Orpiment. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with molybdite?+
Molybdite commonly co-occurs with Molybdenite, Betpakdalite, Quartz. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does molybdite form in?+
Where it forms: In cavities and coating molybdenite in a weathered quartz vein near its contact with topaz-quartz greisen. Working float back to the host body is the standard way to chase a fresh occurrence.
What is molybdite used for?+
Molybdite is used in collector.

Find molybdite on the map

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