Arsenogoyazite is a rare member of the alunite supergroup typically found as small, rhombohedral crystals in the oxidation zones of arsenic-rich ore deposits. Collectors primarily seek this mineral from world-class localities like the Tsumeb Mine, where it forms in association with other rare arsenate minerals.
Is this arsenogoyazite?
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 arsenogoyazite with a known reference. Arsenogoyazite sits at Mohs 4-5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Arsenogoyazite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Arsenogoyazite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: rhombohedral crystals.
Often confused with
Arsenogoyazite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside arsenogoyazite
Minerals reported to co-occur with arsenogoyazite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- SrAl₃(AsO₄)(OH)₆
- Mohs hardness
- 4-5
- Density
- 3.5-3.6 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Rhombohedral Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Polymetallic Ore Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find arsenogoyazite
Classic worldwide localities
- Tsumeb Mine, Namibia
- Schwarzwald, Germany
Field-hunting tip
Look in oxidized hydrothermal polymetallic ore deposits country — that is the host setting where arsenogoyazite typically forms. If you start seeing arseniosiderite, scorodite, tsumcorite in float, you are in the right ground. Field specimens usually show a rhombohedral crystals habit, so train your eye for that shape before scanning the outcrop.





