Heterosite is an iron-rich phosphate mineral that typically forms as an alteration product of triphylite in phosphate-bearing pegmatites. It is prized by collectors for its distinct, intense purple to dark red color, though the color often fades or darkens to brown upon long-term exposure to sunlight.
Is this heterosite?
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 heterosite with a known reference. Heterosite sits at Mohs 4-4.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale purple.
- 3Read the lusterHold the specimen under a strong light. Luster: satiny on fresh surfaces, dull to earthy.
- 4Match the color rangeCompare against the expected color range: brownish black, violet brown, greenish brown, dark brown, dark pink.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: massive, granular, or rarely as distinct prismatic crystals.
Often confused with
Heterosite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside heterosite
Minerals reported to co-occur with heterosite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe□PO₄
- Mohs hardness
- 4-4.5
- Density
- 3.40 g/cm³
- Colors
- Streak
- Pale purple
- Luster
- Satiny on fresh surfaces, dull to earthy
- Transparency
- Translucent to opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Massive, granular, or rarely as distinct prismatic crystals
- Cleavage
- Good on {100}; poor on {010}; surfaces may be curved
- Rarity
- Uncommon
- Uses
- Collector, Decorative
- Host rock
- A secondary mineral in the oxidized zone of complex granite pegmatites, replacing primary phosphate minerals, principally triphylite
Where rockhounds find heterosite
1 mapped spotsClassic worldwide localities
- Fletcher and Palermo #1 mines, near North Groton, Grafton Co., New Hampshire, USA
- Newry, Oxford Co., Maine, USA
- Hill City, Pennington Co., South Dakota, USA
- Haute-Vienne, from near Limoges, Huréaux, and in the La Vilate quarry, near Chanteloube, France
- Hagendorf, and Hühnerkobel, near Zwiesel, Bavaria, Germany
- Norrö pegmatite, on Rånö Island, Sweden
Field-hunting tip
Where it forms: A secondary mineral in the oxidized zone of complex granite pegmatites, replacing primary phosphate minerals, principally triphylite. If you start seeing triphylite, ferrisicklerite in float, you are in the right ground. Typical habit: massive, granular, or rarely as distinct prismatic crystals. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in New Hampshire. Start trip planning there.


