Pararammelsbergite is an uncommon nickel arsenide mineral that occurs primarily in hydrothermal ore deposits. It is frequently confused with its dimorph, rammelsbergite, and often occurs as massive, silver-white material that develops a tarnished, light pinkish hue over time. Collectors should exercise caution due to the significant arsenic content.

Hardness
2-3
Mohs
Luster
Metallic
Streak
Black
Transparency
Opaque

Is this pararammelsbergite?

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 pararammelsbergite with a known reference. Pararammelsbergite sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Pararammelsbergite leaves a black streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Pararammelsbergite typically shows a metallic luster.
  • 4
    Match the color range
    Compare against the expected color range: white, light pink, silver white.
  • 5
    Look at form & habit
    Crystal system: orthorhombic. Typical habit: massive, granular, rarely as small crystals.

Often confused with

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

Often found alongside pararammelsbergite

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

All properties

Chemical formula
NiAs₂
Mohs hardness
2-3
Density
7.1 g/cm³
Streak
Black
Luster
Metallic
Transparency
Opaque
Crystal system
Orthorhombic
Crystal habit
Massive, Granular, Rarely as Small Crystals
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
Hydrothermal Veins, Nickel-cobalt-silver Ore Deposits
Typical price
$20-100 per specimen

Where rockhounds find pararammelsbergite

Classic worldwide localities

  • Ontario, Canada
  • Saxony, Germany
  • Morocco
  • Czech Republic

Field-hunting tip

Look in hydrothermal veins, nickel-cobalt-silver ore deposits country — that is the host setting where pararammelsbergite typically forms. If you start seeing rammelsbergite, gersdorffite, nickeline in float, you are in the right ground. Field specimens usually show a massive, granular, rarely as small crystals habit, so train your eye for that shape before scanning the outcrop.

Common questions

How do you identify pararammelsbergite?+
Mohs hardness is 2-3. It typically shows a metallic luster. The streak is black. Common colors include white, light pink, silver white.
Where is pararammelsbergite found?+
Notable localities include Ontario, Canada; Saxony, Germany; Morocco; Czech Republic.
How much is pararammelsbergite worth?+
Typical asking prices fall in the range of $20-100 per specimen. Quality, size, and provenance can move individual specimens well outside that range.
Is pararammelsbergite safe to handle?+
It contains toxic constituents. Contains arsenic and nickel. Handle with gloves, avoid inhalation of dust, and wash hands thoroughly after handling. Do not ingest. Handle with care, avoid grinding or breathing dust, and store separately.
What rocks look like pararammelsbergite?+
Pararammelsbergite is most often confused with Rammelsbergite, Skutterudite, Nickeline. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with pararammelsbergite?+
Pararammelsbergite commonly co-occurs with Rammelsbergite, Gersdorffite, Nickeline, Cobaltite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does pararammelsbergite form in?+
Pararammelsbergite typically forms in hydrothermal veins, nickel-cobalt-silver ore deposits. Working float back to the host body is the standard way to chase a fresh occurrence.
What is pararammelsbergite used for?+
Pararammelsbergite is used in collector.

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