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, 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.






