Ferrimolybdite is a secondary oxidation product that typically forms as bright yellow, powdery, or fibrous crusts on weathering molybdenite. It is easily identified by its distinctive canary-yellow color and its common occurrence as a soil or vein coating in ore deposits.

Hardness
1-2
Mohs
Luster
Dull
Streak
Pale Yellow
Transparency
Opaque

Is this ferrimolybdite?

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 ferrimolybdite with a known reference. Ferrimolybdite sits at Mohs 1-2 — softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Ferrimolybdite leaves a pale yellow streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Ferrimolybdite typically shows a dull luster.
  • 4
    Match the color range
    Compare against the expected color range: yellow, straw-yellow, canary-yellow.
  • 5
    Look at form & habit
    Crystal system: orthorhombic. Typical habit: fibrous, earthy, powdery, or as encrustations.

Often confused with

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

Often found alongside ferrimolybdite

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

All properties

Chemical formula
Fe₂³⁺(MoO₄)₃·8H₂O
Mohs hardness
1-2
Density
3.0-3.5 g/cm³
Streak
Pale Yellow
Luster
Dull
Transparency
Opaque
Crystal system
Orthorhombic
Crystal habit
Fibrous, Earthy, Powdery, Or as Encrustations
Cleavage
None
Rarity
Common
Uses
Collector, Indicator Mineral
Host rock
Oxidized Zones of Molybdenum-bearing Hydrothermal Deposits
Typical price
$10-60 for small mineral specimens

Where rockhounds find ferrimolybdite

Classic worldwide localities

  • Climax, Colorado, USA
  • Questa, New Mexico, USA
  • Azegour, Morocco
  • Kounrad, Kazakhstan
  • Altai Mountains, Russia

Field-hunting tip

Look in oxidized zones of molybdenum-bearing hydrothermal deposits country — that is the host setting where ferrimolybdite typically forms. If you start seeing molybdenite, limonite, quartz in float, you are in the right ground. Field specimens usually show a fibrous, earthy, powdery, or as encrustations habit, so train your eye for that shape before scanning the outcrop.

Common questions

How do you identify ferrimolybdite?+
Mohs hardness is 1-2. It typically shows a dull luster. The streak is pale yellow. Common colors include yellow, straw-yellow, canary-yellow.
Where is ferrimolybdite found?+
Notable localities include Climax, Colorado, USA; Questa, New Mexico, USA; Azegour, Morocco; Kounrad, Kazakhstan; Altai Mountains, Russia.
How much is ferrimolybdite worth?+
Typical asking prices fall in the range of $10-60 for small mineral specimens. Quality, size, and provenance can move individual specimens well outside that range.
What rocks look like ferrimolybdite?+
Ferrimolybdite is most often confused with Molybdite, Jarosite, Autunite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with ferrimolybdite?+
Ferrimolybdite commonly co-occurs with Molybdenite, Limonite, Quartz, Pyrite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does ferrimolybdite form in?+
Ferrimolybdite typically forms in oxidized zones of molybdenum-bearing hydrothermal deposits. Working float back to the host body is the standard way to chase a fresh occurrence.
What is ferrimolybdite used for?+
Ferrimolybdite is used in collector, indicator mineral.

Find ferrimolybdite on the map

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