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Sulfide

Cinnabar

HgS

The scarlet mercury ore behind vermilion pigment — beautiful and toxic.

Hardness2–2.5
Crystal systemTrigonal
LusterAdamantine
Sp. gravity8–8.2
ClassSulfide
Cinnabar specimen

Cinnabar — Photo: Nessa Eull · CC0

What is Cinnabar?

Cinnabar is mercury sulfide — HgS — and the ore of quicksilver. Its scarlet color made it precious long before mercury had uses: Neolithic burials were dusted with it, Roman triumphs were painted with it, and Chinese lacquer carved it.

It forms in young volcanic and hot-spring systems where mercury-bearing fluids cool near the surface. Almadén in Spain has produced roughly a third of all mercury ever mined.

Handle with respect: mercury compounds are cumulative toxins. Cinnabar is safe to admire in a case — wash your hands after handling and keep it away from heat.

In one sentence: Scarlet, very heavy, very soft — cinnabar is unmistakable where mercury deposits occur.

Physical Properties

The full data table is in the panel alongside. Here’s what those numbers actually mean.

Density. SG ~8.1 — heavier than galena — is diagnostic.

Streak. Bright scarlet streak separates it from dark cuprite and black metacinnabar.

Toxicity. Inhaled dust or mercury vapor is the hazard; intact specimens pose little risk with basic hygiene.

What It’s Used For

Mercury oreEssentially the only commercial source of mercury.
Vermilion pigmentGround cinnabar was the red of illuminated manuscripts and lacquerware.
CautionMercury compounds are toxic — wash hands after handling; never heat.

How to Identify It

Scarlet-red color and streakExtremely heavy (SG ~8.1)Very soft, scratches easilyFound near hot-spring/volcanic mercury districts
Looks like…But differs because…Quick test
RealgarOrange-red, much lighter (SG 3.5), arsenic oreColor & weight
CupriteDarker red, isometric octahedra, in copper depositsOccurrence

Where It’s Found

Notable localities for fine specimens: