Pinchite is a rare mercury oxychloride mineral known primarily from the Terlingua mining district in Texas. It typically occurs as small, transparent, yellow-orange tabular crystals associated with other rare mercury minerals in limestone cavities.
Is this pinchite?
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 pinchite with a known reference. Pinchite sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Pinchite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Pinchite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-orange, colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, subhedral grains.
Often confused with
Pinchite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside pinchite
Minerals reported to co-occur with pinchite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Hg₅Cl₂O₄
- Mohs hardness
- 2-3
- Density
- 7.2 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Subhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Limestone
- Typical price
- $50-500 thumbnail
Where rockhounds find pinchite
Classic worldwide localities
- Terlingua, Texas, USA
Field-hunting tip
Look in hydrothermal veins in limestone country — that is the host setting where pinchite typically forms. If you start seeing calcite, cinnabar, terlinguaite in float, you are in the right ground. Field specimens usually show a tabular crystals, subhedral grains habit, so train your eye for that shape before scanning the outcrop.






