Fernandinite is a rare calcium sodium potassium oxide, typically dull green. It is a filled by a remobilized asphaltite deposit. It is associated with hewettite and quartz. It was first described from Minasragra, 46 km from Cerro de Pasco, Peru.

Hardness
2-3
Mohs
Luster
Submetallic
Streak
Dark green
Transparency
Opaque to translucent

Is this fernandinite?

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 fernandinite with a known reference. Fernandinite 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: dark green.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: submetallic.
  • 4
    Match the color range
    Compare against the expected color range: dark green.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: foliated, massive.

Often confused with

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

Often found alongside fernandinite

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

All properties

Chemical formula
(Ca,Na,K)₀.₉(V⁵⁺,V⁴⁺,Fe²⁺,Ti)₈O₂₀·4H₂O
Mohs hardness
2-3
Density
2.78 g/cm³
Streak
Dark green
Luster
Submetallic
Transparency
Opaque to translucent
Crystal system
Monoclinic
Crystal habit
Foliated, massive
Cleavage
Perfect
Rarity
Rare
Uses
Collector
Host rock
In a rich vanadium deposit in fissures that cut red shales and that were probably filled by a remobilized asphaltite deposit

Where rockhounds find fernandinite

Classic worldwide localities

  • Monument No. 2 mine, Monument Valley, Apache Co., Arizona, USA
  • Cactus Rat mine group, Yellow Cat district, 24 km southeast of Thompson, Grand Co., Utah, USA
  • Spring Creek Mesa area, Uravan district, Montrose Co., Colorado, USA
  • Minasragra, 46 km from Cerro de Pasco, Peru

Field-hunting tip

Where it forms: In a rich vanadium deposit in fissures that cut red shales and that were probably filled by a remobilized asphaltite deposit. If you start seeing hewettite, quartz in float, you are in the right ground. Typical habit: foliated, massive. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify fernandinite?+
Mohs hardness is 2-3. Luster: submetallic. The streak is dark green. Common colors include dark green.
Where is fernandinite found?+
Notable localities include Monument No. 2 mine, Monument Valley, Apache Co., Arizona, USA; Cactus Rat mine group, Yellow Cat district, 24 km southeast of Thompson, Grand Co., Utah, USA; Spring Creek Mesa area, Uravan district, Montrose Co., Colorado, USA; Minasragra, 46 km from Cerro de Pasco, Peru.
Is fernandinite safe to handle?+
Fernandinite contains vanadium. Wash your hands afterwards, never grind or breathe the dust, and store it apart from specimens you handle often.
What rocks look like fernandinite?+
Fernandinite is most often confused with Pascoite, Hewettite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with fernandinite?+
Fernandinite commonly co-occurs with Hewettite, Quartz. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does fernandinite form in?+
Where it forms: In a rich vanadium deposit in fissures that cut red shales and that were probably filled by a remobilized asphaltite deposit. Working float back to the host body is the standard way to chase a fresh occurrence.
What is fernandinite used for?+
Fernandinite is used in collector.

Find fernandinite on the map

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