Philolithite is an extremely rare lead-manganese sulfate mineral primarily found in the Långban mines of Sweden. It typically forms small, medium apple-green dipyramidal crystals associated with complex manganese-rich parageneses. Due to its limited occurrence and scientific rarity, it is highly sought after by advanced systematic mineral collectors.
Is this philolithite?
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 philolithite with a known reference. Philolithite sits at Mohs 3-4, 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: adamantine.
- 4Match the color rangeCompare against the expected color range: green, emerald green.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: encrustations, tabular.
Often confused with
Philolithite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside philolithite
Minerals reported to co-occur with philolithite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₁₂O₆Mn₇(SO₄)(CO₃)₄Cl₄(OH)₁₂
- Mohs hardness
- 3-4
- Density
- 5.91 g/cm³
- Colors
- Streak
- White
- Luster
- Adamantine
- Transparency
- Semitransparent
- Crystal system
- Tetragonal
- Crystal habit
- Encrustations, tabular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Very rare in a metamorphosed Fe–Mn orebody
Where rockhounds find philolithite
Classic worldwide localities
- Långban, Värmland, Sweden
Field-hunting tip
Where it forms: Very rare in a metamorphosed Fe–Mn orebody. If you start seeing lead, copper, mendipite in float, you are in the right ground. Typical habit: encrustations, tabular. Train your eye for that shape before scanning the outcrop.








