Ophirite is a rare calcium magnesium arsenate mineral typically found as small, vibrant yellow platy crystals or crusts. It is primarily known from the Gold Hill district in Utah, where it forms in oxidized zones of arsenic-rich mineral deposits.
Is this ophirite?
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 ophirite with a known reference. Ophirite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ophirite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Ophirite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-orange.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, crusts.
Often confused with
Ophirite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Conichalcite is the harder of the two (Mohs 4.5 vs. 2); streak differs — Ophirite leaves yellow, Conichalcite leaves light green.

How to tell apart: Austinite is the harder of the two (Mohs 4 vs. 2); streak differs — Ophirite leaves yellow, Austinite leaves white.
Often found alongside ophirite
Minerals reported to co-occur with ophirite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Mg₃(H₂O)₄(AsO₄)₂F₄
- Mohs hardness
- 2
- Density
- 4.26 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Crusts
- Cleavage
- Perfect
- Fluorescence
- Bright Yellow Under UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Arsenic-rich Hydrothermal Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find ophirite
Classic worldwide localities
- Gold Hill Mine, Utah, USA
Field-hunting tip
Look in oxidized arsenic-rich hydrothermal deposits country — that is the host setting where ophirite typically forms. If you start seeing arsenopyrite, scorodite, quartz in float, you are in the right ground. Field specimens usually show a platy crystals, crusts habit, so train your eye for that shape before scanning the outcrop.



