Eylettersite is a rare phosphate-sulfate mineral member of the woodhouseite group, primarily known as a secondary mineral in uranium-bearing pegmatites. It typically occurs as minute, crust-like or massive aggregates and is of interest primarily to advanced systematic mineral collectors due to its radioactive nature and scarcity.
Is this eylettersite?
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 eylettersite with a known reference. Eylettersite sits at Mohs 5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Eylettersite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Eylettersite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, yellowish.
- 5Look at form & habitCrystal system: trigonal. Typical habit: microscopic crystals, massive, crusts.
Often confused with
Eylettersite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside eylettersite
Minerals reported to co-occur with eylettersite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Th(PO₄,SO₄)₂(OH,H₂O)₄
- Mohs hardness
- 5
- Density
- 3.31 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Microscopic Crystals, Massive, Crusts
- Cleavage
- None Observed
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find eylettersite
Classic worldwide localities
- Kobokobo, Democratic Republic of the Congo
- Lachaux, France
Field-hunting tip
Look in granite pegmatites country — that is the host setting where eylettersite typically forms. If you start seeing meta-autunite, phosphuranylite, beryl in float, you are in the right ground. Field specimens usually show a microscopic crystals, massive, crusts habit, so train your eye for that shape before scanning the outcrop.





