Reddingite is a rare phosphate mineral typically found in phosphate-rich zones of granite pegmatites. It forms short, blocky, prismatic crystals or compact granular masses that are prized by advanced collectors of phosphate minerals.

Hardness
3-3.5
Mohs
Luster
Vitreous to subresinous
Streak
White
Transparency
Transparent to translucent

Is this reddingite?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch reddingite with a known reference. Reddingite sits at Mohs 3-3.5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: white.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous to subresinous.
  • 4
    Match the color range
    Compare against the expected color range: white, yellowish white, colorless, reddish brown, dark brown.
  • 5
    Look at form & habit
    Crystal system: orthorhombic. Typical habit: crystalline, granular.

Often confused with

Reddingite vs. its common look-alikes, and how to tell them apart in the field.

Often found alongside reddingite

Minerals reported to co-occur with reddingite. Spotting these in float or country rock is a strong cue you are in the right ground.

All properties

Chemical formula
Mn²⁺₃(PO₄)₂·3H₂O
Mohs hardness
3-3.5
Density
3.10-3.24 g/cm³
Streak
White
Luster
Vitreous to subresinous
Transparency
Transparent to translucent
Crystal system
Orthorhombic
Crystal habit
Crystalline, granular
Cleavage
On {010}, poor
Rarity
Rare
Uses
Collector
Host rock
A rare secondary hydrothermal alteration product in zoned complex granite pegmatites

Where rockhounds find reddingite

Classic worldwide localities

  • Branchville, in the town of Redding, Fairfield Co., Connecticut (type locality)

Field-hunting tip

Where it forms: A rare secondary hydrothermal alteration product in zoned complex granite pegmatites. If you start seeing dickinsonite, triploidite, triplite in float, you are in the right ground. Typical habit: crystalline, granular. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify reddingite?+
Mohs hardness is 3-3.5. Luster: vitreous to subresinous. The streak is white. Common colors include white, yellowish white, colorless, reddish brown.
Where is reddingite found?+
Notable localities include Branchville, in the town of Redding, Fairfield Co., Connecticut (type locality).
What rocks look like reddingite?+
Reddingite is most often confused with Phosphosiderite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with reddingite?+
Reddingite commonly co-occurs with Dickinsonite, Triploidite, Triplite, Lithiophilite, Fairfieldite, Eosphorite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does reddingite form in?+
Where it forms: A rare secondary hydrothermal alteration product in zoned complex granite pegmatites. Working float back to the host body is the standard way to chase a fresh occurrence.
What is reddingite used for?+
Reddingite is used in collector.

Find reddingite on the map

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