Sigloite is a rare phosphate mineral typically found as a secondary oxidation product in tin-bearing hydrothermal deposits. It is most frequently encountered as small, tabular, yellowish crystals often associated with other phosphate minerals like vauxite and paravauxite.
Is this sigloite?
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 sigloite with a known reference. Sigloite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to pearly.
- 4Match the color rangeCompare against the expected color range: brown, light brown, light yellow, straw yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: pseudomorphous.
Often confused with
Sigloite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside sigloite
Minerals reported to co-occur with sigloite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- FeAl₂(PO₄)₂(OH)₃·7H₂O
- Mohs hardness
- 3
- Density
- 2.35 g/cm³
- Streak
- White
- Luster
- Vitreous to pearly
- Transparency
- Semitransparent
- Crystal system
- Triclinic
- Crystal habit
- Pseudomorphous
- Cleavage
- On {010}, perfect; on {001}, good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare late-stage secondary mineral, formed by oxidation of vauxite, in open fractures cutting cassiterite veins in a hydrothermal tin deposit
Where rockhounds find sigloite
Classic worldwide localities
- Found in the Siglo XX mine, Llallagua, Potosí, Bolivia
Field-hunting tip
Where it forms: A rare late-stage secondary mineral, formed by oxidation of vauxite, in open fractures cutting cassiterite veins in a hydrothermal tin deposit. If you start seeing wavellite, metavauxite, crandallite in float, you are in the right ground. Typical habit: pseudomorphous. Train your eye for that shape before scanning the outcrop.







