Rhodarsenide is a rare rhodium arsenide mineral that occurs primarily as small, metallic grains within platinum-group mineral assemblages. It is most frequently found in alluvial deposits derived from ultramafic rocks or in chromitite layers. Collectors prize it as a micro-mineral due to its extreme scarcity and association with platinum-group elements.

Hardness
4-5
Mohs
Luster
Metallic
Transparency
Opaque

Is this rhodarsenide?

4-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 rhodarsenide with a known reference. Rhodarsenide sits at Mohs 4-5, softer than the next harder reference, harder than the previous one.
  • 2
    Read the luster
    Hold the specimen under a strong light. Luster: metallic.
  • 3
    Match the color range
    Compare against the expected color range: brown.
  • 4
    Look at form & habit
    Crystal system: orthorhombic. Typical habit: inclusions.

Often confused with

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

Often found alongside rhodarsenide

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

All properties

Chemical formula
Rh₂As
Mohs hardness
4-5
Density
11.27-11.32 g/cm³
Colors
Luster
Metallic
Transparency
Opaque
Crystal system
Orthorhombic
Crystal habit
Inclusions
Rarity
Rare
Uses
Collector
Host rock
In fluvial placers in a river draining a chromitite-bearing ophiolite (TL)

Where rockhounds find rhodarsenide

Classic worldwide localities

  • Srebrnica River, near Veluce, central Serbia (TL)
  • Pustaya River placer, Kamchatka Peninsula, eastern Russia and Simonovsky Brook, tributary of the Malaya Krokhalevka River, Salair Range, Eastern Siberia, Russia
  • Onverwacht pipe, eastern Bushveld Complex, South Africa (eluvial)

Field-hunting tip

Where it forms: In fluvial placers in a river draining a chromitite-bearing ophiolite (TL). If you start seeing pt-fe alloys, ru-os-ir alloys, hollingworthite in float, you are in the right ground. Typical habit: inclusions. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify rhodarsenide?+
Mohs hardness is 4-5. Luster: metallic. Common colors include brown.
Where is rhodarsenide found?+
Notable localities include Srebrnica River, near Veluce, central Serbia (TL); Pustaya River placer, Kamchatka Peninsula, eastern Russia and Simonovsky Brook, tributary of the Malaya Krokhalevka River, Salair Range, Eastern Siberia, Russia; Onverwacht pipe, eastern Bushveld Complex, South Africa (eluvial).
Is rhodarsenide safe to handle?+
Rhodarsenide contains arsenic and calls for real care. Contains arsenic, which is toxic; avoid inhaling dust or handling with bare hands without washing thoroughly.
What rocks look like rhodarsenide?+
Rhodarsenide is most often confused with Sperrylite, Arsenopalladinite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with rhodarsenide?+
Rhodarsenide commonly co-occurs with Pt-Fe alloys, Ru-Os-Ir alloys, Hollingworthite, Irarsite, Sperrylite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does rhodarsenide form in?+
Where it forms: In fluvial placers in a river draining a chromitite-bearing ophiolite (TL). Working float back to the host body is the standard way to chase a fresh occurrence.
What is rhodarsenide used for?+
Rhodarsenide is used in collector.

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