Molybdenite is the primary ore of molybdenum, easily identified by its metallic lead-gray color, greasy feel, and perfect cleavage that creates flexible, non-elastic plates. It is significantly denser than its look-alike, graphite, and produces a characteristic greenish-gray streak on unglazed porcelain.
Is this molybdenite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch molybdenite with a known reference. Molybdenite sits at Mohs 1-1.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: bluish gray.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: lead-gray, bluish-gray, black, gray.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: disseminated, foliated, massive.
Often confused with
Molybdenite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Molybdenite leaves bluish gray, Graphite leaves black to steel-gray, shining.

How to tell apart: Hematite is the harder of the two (Mohs 5-6 vs. 1-1.5); streak differs, so Molybdenite leaves bluish gray, Hematite leaves cherry-red or reddish brown.
Often found alongside molybdenite
Minerals reported to co-occur with molybdenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- MoS₂
- Mohs hardness
- 1-1.5
- Density
- 4.62-4.73 g/cm³
- Streak
- Bluish gray
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Disseminated, foliated, massive
- Cleavage
- Perfect on {0001}
- Rarity
- Common
- Uses
- Industrial, Collector
- Host rock
- In high-temperature hydrothermal veins
Where rockhounds find molybdenite
16 mapped spotsClassic worldwide localities
- Frankford quarry, Philadelphia, Pennsylvania, USA
- Fine crystals occur, in the USA, at the Crown Point mine, Lake Chelan, Chelan Co., Washington
- Temiskaming district, and in Aldfield Township, Quebec, Canada
- Raade, near Moss, and at Vennesla, near Arendal, Norway
- Adun-Chilon Mountains, south of Nerchinsk, Transbaikal, Russia
- Miass, Ilmen Mountains, Southern Ural Mountains, Russia
Field-hunting tip
Where it forms: In high-temperature hydrothermal veins. If you start seeing chalcopyrite in float, you are in the right ground. Typical habit: disseminated, foliated, massive. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Utah, Maine, New Mexico. Start trip planning there.



