Kuramite is a rare copper-tin sulfide mineral discovered in the Kurama Mountains. It typically occurs as small, metallic grains within hydrothermal ore deposits and is highly prized by advanced mineral collectors for its scarcity.

Hardness
5
Mohs
Luster
Metallic
Streak
Metallic
Transparency
Opaque

Is this kuramite?

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 kuramite with a known reference. Kuramite sits at Mohs 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: metallic.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: metallic.
  • 4
    Match the color range
    Compare against the expected color range: gray, steel gray.
  • 5
    Look at form & habit
    Crystal system: tetragonal. Typical habit: inclusions, microscopic crystals.

Often confused with

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

Often found alongside kuramite

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

All properties

Chemical formula
Cu₃SnS₄
Mohs hardness
5
Density
4.56 g/cm³
Streak
Metallic
Luster
Metallic
Transparency
Opaque
Crystal system
Tetragonal
Crystal habit
Inclusions, microscopic crystals
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
In gold–sulfide–quartz veins, as inclusions in goldfieldite (Kochbulak deposit, Uzbekistan)

Where rockhounds find kuramite

Classic worldwide localities

  • Bisbee, Cochise Co., Arizona, USA
  • Zuni mine, near Silverton, San Juan Co., Colorado, USA
  • Gold Crater district, Nye Co., Nevada, USA
  • Kochbulak gold deposit, Chatkal-Kuramin Mountains, eastern Uzbekistan (type locality)
  • Gunheath china clay pit, St. Austell, Cornwall, England

Field-hunting tip

Where it forms: In gold–sulfide–quartz veins, as inclusions in goldfieldite (Kochbulak deposit, Uzbekistan). If you start seeing goldfieldite, famatinite, hessite in float, you are in the right ground. Typical habit: inclusions, microscopic crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify kuramite?+
Mohs hardness is 5. Luster: metallic. The streak is metallic. Common colors include gray, steel gray.
Where is kuramite found?+
Notable localities include Bisbee, Cochise Co., Arizona, USA; Zuni mine, near Silverton, San Juan Co., Colorado, USA; Gold Crater district, Nye Co., Nevada, USA; Kochbulak gold deposit, Chatkal-Kuramin Mountains, eastern Uzbekistan (type locality); Gunheath china clay pit, St. Austell, Cornwall, England.
Is kuramite safe to handle?+
Kuramite contains copper. Contains copper and sulfur; handle with care and wash hands thoroughly after handling. Do not ingest or inhale dust.
What rocks look like kuramite?+
Kuramite is most often confused with Stannite, Briartite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with kuramite?+
Kuramite commonly co-occurs with Goldfieldite, Famatinite, Hessite, Petzite, Sylvanite, Altaite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does kuramite form in?+
Where it forms: In gold–sulfide–quartz veins, as inclusions in goldfieldite (Kochbulak deposit, Uzbekistan). Working float back to the host body is the standard way to chase a fresh occurrence.
What is kuramite used for?+
Kuramite is used in collector.

Find kuramite on the map

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