Radtkeite is a rare mercury halide sulfide mineral typically found as small, orange crystals in oxidized mercury deposits. It is specifically known from the McDermitt mine in Nevada, often occurring as encrustations associated with other mercury-bearing minerals. Because it is highly rare and contains mercury, it is sought after primarily by advanced mineral collectors.

Hardness
2-3
Mohs
Luster
Nearly adamantine (synthetic)
Streak
Yellow-orange, blackening on exposure to light
Transparency
Opaque to translucent

Is this radtkeite?

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 radtkeite with a known reference. Radtkeite 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. Streak: yellow-orange, blackening on exposure to light.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: nearly adamantine (synthetic).
  • 4
    Match the color range
    Compare against the expected color range: orange, bright yellow orange.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: microscopic crystals.

Often confused with

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

Often found alongside radtkeite

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

All properties

Chemical formula
Hg₃S₂ClI
Mohs hardness
2-3
Density
7.0 g/cm³
Colors
OrangeBright yellow orange
Streak
Yellow-orange, blackening on exposure to light
Luster
Nearly adamantine (synthetic)
Transparency
Opaque to translucent
Crystal system
Monoclinic
Crystal habit
Microscopic crystals
Cleavage
Perfect on {010}; very good on {001}; very good on {100}
Rarity
Rare
Uses
Collector
Host rock
In tuffaceous rhyolitic lake-bed sediments, formed as a reaction product between halide-bearing hydrothermal solutions and cinnabar or corderoite

Where rockhounds find radtkeite

Classic worldwide localities

  • McDermitt mercury mine, Opalite district, Humboldt Co., Nevada, USA

Field-hunting tip

Where it forms: In tuffaceous rhyolitic lake-bed sediments, formed as a reaction product between halide-bearing hydrothermal solutions and cinnabar or corderoite. If you start seeing cinnabar, corderoite, quartz in float, you are in the right ground. Typical habit: microscopic crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify radtkeite?+
Mohs hardness is 2-3. Luster: nearly adamantine (synthetic). The streak is yellow-orange, blackening on exposure to light. Common colors include orange, bright yellow orange.
Where is radtkeite found?+
Notable localities include McDermitt mercury mine, Opalite district, Humboldt Co., Nevada, USA.
Is radtkeite safe to handle?+
Radtkeite contains mercury and calls for real care. Contains mercury; handle with caution, avoid inhaling dust, and wash hands thoroughly after contact.
What rocks look like radtkeite?+
Radtkeite is most often confused with Cinnabar, Calomel, Kadyrelite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with radtkeite?+
Radtkeite commonly co-occurs with Cinnabar, Corderoite, Quartz, Gypsum. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does radtkeite form in?+
Where it forms: In tuffaceous rhyolitic lake-bed sediments, formed as a reaction product between halide-bearing hydrothermal solutions and cinnabar or corderoite. Working float back to the host body is the standard way to chase a fresh occurrence.
What is radtkeite used for?+
Radtkeite is used in collector.

Find radtkeite on the map

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