Bismite is a rare secondary mineral that typically forms as a yellowish earthy crust or powdery aggregate resulting from the oxidation of native bismuth. It is found most commonly in the oxidized parts of hydrothermal veins and is prized by mineral collectors for its high density and associations with other bismuth-bearing species.

Hardness
4.5
Mohs
Luster
Subadamantine to dull, earthy
Streak
Gray to yellow
Transparency
Transparent in very small fragments

Is this bismite?

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 bismite with a known reference. Bismite sits at Mohs 4.5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: gray to yellow.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: subadamantine to dull, earthy.
  • 4
    Match the color range
    Compare against the expected color range: green yellow, gray green, yellow.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: earthy, pulverulent, scaly.

Often confused with

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

Often found alongside bismite

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

All properties

Chemical formula
Bi₂O₃
Mohs hardness
4.5
Density
8.64-9.22 g/cm³
Streak
Gray to yellow
Luster
Subadamantine to dull, earthy
Transparency
Transparent in very small fragments
Crystal system
Monoclinic
Crystal habit
Earthy, pulverulent, scaly
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
An oxidation product of bismuth

Where rockhounds find bismite

Classic worldwide localities

  • Harding mine, Dixon, Taos Co., New Mexico, USA
  • Victor mine, Rincon, and in a number of the pegmatites at Pala, San Diego Co., and near Baker, San Bernardino Co., California, USA
  • Missouri mine, Park Co., Colorado, USA
  • Colavi, at Tazna, and Llallagua, Bolivia
  • Ebisu mine, Gifu Prefecture, Japan

Field-hunting tip

Where it forms: An oxidation product of bismuth. If you start seeing bismuth, bismutite, cassiterite in float, you are in the right ground. Typical habit: earthy, pulverulent, scaly. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify bismite?+
Mohs hardness is 4.5. Luster: subadamantine to dull, earthy. The streak is gray to yellow. Common colors include green yellow, gray green, yellow.
Where is bismite found?+
Notable localities include Harding mine, Dixon, Taos Co., New Mexico, USA; Victor mine, Rincon, and in a number of the pegmatites at Pala, San Diego Co., and near Baker, San Bernardino Co., California, USA; Missouri mine, Park Co., Colorado, USA; Colavi, at Tazna, and Llallagua, Bolivia; Ebisu mine, Gifu Prefecture, Japan.
Is bismite safe to handle?+
Contains bismuth, which is generally considered to have low toxicity, but proper handling is advised; avoid inhaling dust and wash hands after handling.
What rocks look like bismite?+
Bismite is most often confused with Bismutite, Bindheimite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with bismite?+
Bismite commonly co-occurs with Bismuth, Bismutite, Cassiterite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does bismite form in?+
Where it forms: An oxidation product of bismuth. Working float back to the host body is the standard way to chase a fresh occurrence.
What is bismite used for?+
Bismite is used in collector.

Find bismite on the map

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

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