Szymańskiite is a rare mercury nickel carbonate that forms sprays of euhedral to subhedral prismatic crystals. It was approved as a distinct mineral species in 1989. It was first described from the Clear Creek claim, San Benito Co., California, USA.

Hardness
3
Mohs
Luster
Vitreous
Streak
Pale blue
Transparency
Transparent

Is this szymańskiite?

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 szymańskiite with a known reference. Szymańskiite sits at Mohs 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: pale blue.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: blue gray, blue green, black.
  • 5
    Look at form & habit
    Crystal system: hexagonal. Typical habit: sprays of euhedral to subhedral prismatic crystals.

Often confused with

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

Often found alongside szymańskiite

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

All properties

Chemical formula
Hg₁₆Ni₆(CO₃)₁₂(OH)₁₂(H₃O)₈·3H₂O
Mohs hardness
3
Density
4.86 g/cm³
Streak
Pale blue
Luster
Vitreous
Transparency
Transparent
Crystal system
Hexagonal
Crystal habit
Sprays of euhedral to subhedral prismatic crystals
Cleavage
{1010}, poor
Rarity
Rare
Uses
Collector
Host rock
A very rare secondary mineral in the oxidized zone of a mercury–nickel-bearing sulfide deposit in silicate–carbonate rock hydrothermally altered from serpentinite

Where rockhounds find szymańskiite

Classic worldwide localities

  • Clear Creek claim, near the Clear Creek mercury mine, New Idria district, San Benito Co., California, USA

Field-hunting tip

Where it forms: A very rare secondary mineral in the oxidized zone of a mercury–nickel-bearing sulfide deposit in silicate–carbonate rock hydrothermally altered from serpentinite. If you start seeing cinnabar, montroydite, mercury in float, you are in the right ground. Typical habit: sprays of euhedral to subhedral prismatic crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify szymańskiite?+
Mohs hardness is 3. Luster: vitreous. The streak is pale blue. Common colors include blue gray, blue green, black.
Where is szymańskiite found?+
Notable localities include Clear Creek claim, near the Clear Creek mercury mine, New Idria district, San Benito Co., California, USA.
Is szymańskiite safe to handle?+
Szymańskiite contains mercury and nickel and calls for real care. Contains mercury; handle with care, avoid inhalation of dust or ingestion, and wash hands thoroughly after handling.
What rocks look like szymańskiite?+
Szymańskiite is most often confused with Variscite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with szymańskiite?+
Szymańskiite commonly co-occurs with Cinnabar, Montroydite, Mercury, Edgarbaileyite, Millerite, Quartz. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does szymańskiite form in?+
Where it forms: A very rare secondary mineral in the oxidized zone of a mercury–nickel-bearing sulfide deposit in silicate–carbonate rock hydrothermally altered from serpentinite. Working float back to the host body is the standard way to chase a fresh occurrence.
What is szymańskiite used for?+
Szymańskiite is used in collector.

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