Strengite is an attractive iron phosphate mineral often sought by collectors for its vibrant violet to raspberry-red colors. It typically forms as radiating spherical, botryoidal, or drusy aggregates, and is commonly found in the oxidized zones of iron-rich mineral deposits.
Is this strengite?
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 strengite with a known reference. Strengite sits at Mohs 3.5-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Strengite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Strengite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: red, violet, pink, magenta, colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: botryoidal, crusts, radial aggregates, or prismatic crystals.
Often confused with
Strengite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside strengite
Minerals reported to co-occur with strengite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- FePO₄·2H₂O
- Mohs hardness
- 3.5-4
- Density
- 2.87 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Botryoidal, Crusts, Radial Aggregates, Or Prismatic Crystals
- Cleavage
- Good On {010}
- Rarity
- Uncommon
- Uses
- Collector, Ornamental
- Host rock
- Phosphate-rich Hydrothermal Veins in Granitic Pegmatites or Secondary Gossans
- Typical price
- $15-150 thumbnail, $50-500 cabinet specimen
Where rockhounds find strengite
Classic worldwide localities
- Pleystein, Germany
- Minas Gerais, Brazil
- Rockbridge County, Virginia, USA
- Yukon Territory, Canada
Field-hunting tip
Look in phosphate-rich hydrothermal veins in granitic pegmatites or secondary gossans country — that is the host setting where strengite typically forms. If you start seeing vivianite, cacoxenite, rockbridgeite in float, you are in the right ground. Field specimens usually show a botryoidal, crusts, radial aggregates, or prismatic crystals habit, so train your eye for that shape before scanning the outcrop.







