Pennantite is a manganese-rich member of the chlorite group that typically forms as soft, micaceous plates. Collectors prize it for its distinct brown to orange-brown color, which differentiates it from the common green iron-magnesium chlorites. It is most frequently found in metamorphosed manganese deposits where it occurs alongside minerals like hausmannite.
Is this pennantite?
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 pennantite with a known reference. Pennantite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Pennantite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Pennantite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: brown, reddish-brown, orange-brown.
- 5Look at form & habitCrystal system: triclinic. Typical habit: platy crystals, foliated masses, hexagonal-shaped plates.
Often confused with
Pennantite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside pennantite
Minerals reported to co-occur with pennantite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Mn,Al)₆(Si,Al)₄O₁₀(OH)₈
- Mohs hardness
- 2
- Density
- 3.0-3.1 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Platy Crystals, Foliated Masses, Hexagonal-shaped Plates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Manganese-rich Hydrothermal Deposits
- Typical price
- $20-150 per specimen depending on size and crystal definition
Where rockhounds find pennantite
Classic worldwide localities
- Gwenlais Quarry, Wales
- Franklin, New Jersey, USA
- Langban, Sweden
Field-hunting tip
Look in manganese-rich hydrothermal deposits country — that is the host setting where pennantite typically forms. If you start seeing quartz, calcite, hausmannite in float, you are in the right ground. Field specimens usually show a platy crystals, foliated masses, hexagonal-shaped plates habit, so train your eye for that shape before scanning the outcrop.







