Polhemusite is an extremely rare zinc-mercury sulfide mineral typically found in low-temperature hydrothermal deposits. It is best identified by its association with mercury minerals and its characteristic occurrence as minute, metallic, tetragonal tabular crystals.
Is this polhemusite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch polhemusite with a known reference. Polhemusite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Polhemusite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Polhemusite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, gray.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: tabular crystals, massive.
Often confused with
Polhemusite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Streak differs — Polhemusite leaves white, Sphalerite leaves white to yellow-brown; luster reads metallic on Polhemusite and resinous to submetallic on Sphalerite.

How to tell apart: Polhemusite is noticeably harder (Mohs 3.5 vs. 2-2.5); streak differs — Polhemusite leaves white, Cinnabar leaves scarlet; luster reads metallic on Polhemusite and adamantine on Cinnabar.
Often found alongside polhemusite
Minerals reported to co-occur with polhemusite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Zn,Hg)S
- Mohs hardness
- 3.5
- Density
- 4.96 g/cm³
- Streak
- White
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Tabular Crystals, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $50-300 per specimen
Where rockhounds find polhemusite
Classic worldwide localities
- Mercur District, Utah, USA
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where polhemusite typically forms. If you start seeing cinnabar, realgar, calcite in float, you are in the right ground. Field specimens usually show a tabular crystals, massive habit, so train your eye for that shape before scanning the outcrop.



