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, so 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, so 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, 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.



