Gerstleyite is an extremely rare sulfosalt mineral found primarily in borate deposits in California. It typically occurs as reddish-orange crusts or small fibrous aggregates associated with colemanite and realgar.
Is this gerstleyite?
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 gerstleyite with a known reference. Gerstleyite sits at Mohs 1.5-2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Gerstleyite leaves a orange streak.
- 3Read the lusterHold the specimen under a strong light. Gerstleyite typically shows a resinous luster.
- 4Match the color rangeCompare against the expected color range: red, orange, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: massive, crusts, or radiating fibrous aggregates.
Often confused with
Gerstleyite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Streak differs — Gerstleyite leaves orange, Realgar leaves orange-red.

How to tell apart: Streak differs — Gerstleyite leaves orange, Cinnabar leaves scarlet; luster reads resinous on Gerstleyite and adamantine on Cinnabar.
Often found alongside gerstleyite
Minerals reported to co-occur with gerstleyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂HgSb₈S₁₆·2H₂O
- Mohs hardness
- 1.5-2
- Density
- 3.5 g/cm³
- Streak
- Orange
- Luster
- Resinous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Massive, Crusts, Or Radiating Fibrous Aggregates
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Evaporite Deposits in Borate Mines
- Typical price
- $50-300 per specimen
Where rockhounds find gerstleyite
Classic worldwide localities
- Boron, California, USA
Field-hunting tip
Look in evaporite deposits in borate mines country — that is the host setting where gerstleyite typically forms. If you start seeing colemanite, ulexite, realgar in float, you are in the right ground. Field specimens usually show a massive, crusts, or radiating fibrous aggregates habit, so train your eye for that shape before scanning the outcrop.



