Huizingite-(Al) is an extremely rare ammonium-aluminum sulfate mineral first identified in the Hagendorf-Sud pegmatite of Bavaria. It typically occurs as tiny, distinct yellow tabular crystals within cavities in phosphate-rich pegmatite environments. Collectors usually encounter this only as micro-mount specimens due to the rarity of its discovery sites.
Is this huizingite-(al)?
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 huizingite-(al) with a known reference. Huizingite-(Al) 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. Huizingite-(Al) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Huizingite-(Al) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-orange.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals.
Often confused with
Huizingite-(Al) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside huizingite-(al)
Minerals reported to co-occur with huizingite-(al). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (NH₄)₃Al(SO₄)₂(OH)₂·H₂O
- Mohs hardness
- 2-3
- Density
- 2.25 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Phosphate-rich Granitic Pegmatites
- Typical price
- $100-500 per specimen
Where rockhounds find huizingite-(al)
Classic worldwide localities
- Hagendorf-Sud pegmatite, Germany
Field-hunting tip
Look in phosphate-rich granitic pegmatites country — that is the host setting where huizingite-(al) typically forms. If you start seeing arcanite, mascagnite, tschermigite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.




