Coyoteite is a very rare sulfide mineral found as small, black, platy crystals. It is primarily known from the Coyote Peak diatreme in California where it occurs in vugs within alkaline igneous rocks. Collectors typically find it associated with other sulfide minerals in small, specialized mineralogical collections.

Hardness
~1.5
Mohs
Luster
Metallic
Streak
Black
Transparency
Opaque

Is this coyoteite?

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 coyoteite with a known reference. Coyoteite sits at Mohs ~1.5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: black.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: metallic.
  • 4
    Match the color range
    Compare against the expected color range: black.
  • 5
    Look at form & habit
    Crystal system: triclinic. Typical habit: irregular grains.

Often confused with

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

Often found alongside coyoteite

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

All properties

Chemical formula
NaFe₃S₅·2H₂O
Mohs hardness
~1.5
Density
2.5-2.63 g/cm³
Colors
Streak
Black
Luster
Metallic
Transparency
Opaque
Crystal system
Triclinic
Crystal habit
Irregular grains
Cleavage
Perfect on {111}
Rarity
Rare
Uses
Collector
Host rock
With rare iron sulfides in small pegmatitic clots thought to have crystallized late in the consolidation of the Coyote Peak intrusive, an alkalic mafic diatreme

Where rockhounds find coyoteite

Classic worldwide localities

  • Coyote Peak, near Orick, Humboldt Co., California, USA (type locality)

Field-hunting tip

Where it forms: With rare iron sulfides in small pegmatitic clots thought to have crystallized late in the consolidation of the Coyote Peak intrusive, an alkalic mafic diatreme. If you start seeing pyrrhotite, djerfisherite, rasvumite in float, you are in the right ground. Typical habit: irregular grains. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify coyoteite?+
Mohs hardness is ~1.5. Luster: metallic. The streak is black. Common colors include black.
Where is coyoteite found?+
Notable localities include Coyote Peak, near Orick, Humboldt Co., California, USA (type locality).
What rocks look like coyoteite?+
Coyoteite is most often confused with Valleriite, Cubanite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with coyoteite?+
Coyoteite commonly co-occurs with Pyrrhotite, Djerfisherite, Rasvumite, Bartonite, Erdite, Phlogopite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does coyoteite form in?+
Where it forms: With rare iron sulfides in small pegmatitic clots thought to have crystallized late in the consolidation of the Coyote Peak intrusive, an alkalic mafic diatreme. Working float back to the host body is the standard way to chase a fresh occurrence.
What is coyoteite used for?+
Coyoteite is used in collector.

Find coyoteite on the map

RockHoundR shows mapped rockhounding spots, access rules, and lets you log every find.

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