Oosterboschite is an exceptionally rare palladium-copper selenide mineral found in the oxidation zones of specific cobalt-copper deposits. It typically occurs as microscopic grains embedded within larger mineral masses, requiring professional micro-analysis for definitive identification.

Hardness
3-3.5
Mohs
Luster
Metallic
Streak
Black
Transparency
Opaque

Is this oosterboschite?

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 oosterboschite with a known reference. Oosterboschite sits at Mohs 3-3.5 — softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Oosterboschite leaves a black streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Oosterboschite typically shows a metallic luster.
  • 4
    Match the color range
    Compare against the expected color range: white, pale yellow.
  • 5
    Look at form & habit
    Crystal system: orthorhombic. Typical habit: anhedral to subhedral grains and inclusions.

Often confused with

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

Often found alongside oosterboschite

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

All properties

Chemical formula
(Pd,Cu)₇Se₅
Mohs hardness
3-3.5
Density
9.18 g/cm³
Streak
Black
Luster
Metallic
Transparency
Opaque
Crystal system
Orthorhombic
Crystal habit
Anhedral to Subhedral Grains and Inclusions
Cleavage
None
Rarity
Rare
Uses
Collector, Research
Host rock
Sedimentary-hosted Copper-cobalt-uranium Deposits
Typical price
Expensive, primarily sold to specialized mineral researchers and high-end systematic collectors.

Where rockhounds find oosterboschite

Classic worldwide localities

  • Musonoi mine, Kolwezi, Democratic Republic of the Congo

Field-hunting tip

Look in sedimentary-hosted copper-cobalt-uranium deposits country — that is the host setting where oosterboschite typically forms. If you start seeing selenide minerals, uraninite, hematite in float, you are in the right ground. Field specimens usually show a anhedral to subhedral grains and inclusions habit, so train your eye for that shape before scanning the outcrop.

Common questions

How do you identify oosterboschite?+
Mohs hardness is 3-3.5. It typically shows a metallic luster. The streak is black. Common colors include white, pale yellow.
Where is oosterboschite found?+
Notable localities include Musonoi mine, Kolwezi, Democratic Republic of the Congo.
How much is oosterboschite worth?+
Typical asking prices fall in the range of Expensive, primarily sold to specialized mineral researchers and high-end systematic collectors.. Quality, size, and provenance can move individual specimens well outside that range.
Is oosterboschite safe to handle?+
It contains toxic constituents. Contains selenium, which can be toxic if ingested or inhaled as dust; handle with care and wash hands after handling. Handle with care, avoid grinding or breathing dust, and store separately.
What rocks look like oosterboschite?+
Oosterboschite is most often confused with Trogtalite, Chrisstanleyite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with oosterboschite?+
Oosterboschite commonly co-occurs with Selenide minerals, Uraninite, Hematite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does oosterboschite form in?+
Oosterboschite typically forms in sedimentary-hosted copper-cobalt-uranium deposits. Working float back to the host body is the standard way to chase a fresh occurrence.
What is oosterboschite used for?+
Oosterboschite is used in collector, research.

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