Eglestonite is a rare mercury oxychloride mineral that is most famous for its occurrence in the Terlingua mining district of Texas. It typically presents as small, brilliant yellow-orange or yellow-brown crystals that quickly darken to a dull brownish-black upon exposure to light, making fresh, bright specimens highly sought after by collectors.
Is this eglestonite?
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 eglestonite with a known reference. Eglestonite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Eglestonite leaves a yellowish-white streak.
- 3Read the lusterHold the specimen under a strong light. Eglestonite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-brown, orange, brown.
- 5Look at form & habitCrystal system: cubic. Typical habit: dodecahedral crystals, massive, crusts.
Often confused with
Eglestonite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside eglestonite
Minerals reported to co-occur with eglestonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Hg₄Cl₂O
- Mohs hardness
- 2.5
- Density
- 8.32 g/cm³
- Streak
- Yellowish-white
- Luster
- Adamantine
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Dodecahedral Crystals, Massive, Crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Mercury-rich Hydrothermal Deposits
- Typical price
- $50-500 thumbnail
Where rockhounds find eglestonite
Classic worldwide localities
- Terlingua, Texas, USA
- Idrija, Slovenia
- Almadén, Spain
- Mount Diablo, California, USA
Field-hunting tip
Look in mercury-rich hydrothermal deposits country — that is the host setting where eglestonite typically forms. If you start seeing calomel, terlinguaite, cinnabar in float, you are in the right ground. Field specimens usually show a dodecahedral crystals, massive, crusts habit, so train your eye for that shape before scanning the outcrop.



