Nizamoffite is a very rare phosphate mineral typically found as small, clear, equant crystals within phosphate-rich zones of granite pegmatites. It is best identified by its association with secondary phosphate minerals and its distinct crystal form in specialized pegmatite assemblages.

Hardness
~3.5
Mohs
Luster
Vitreous
Streak
White
Transparency
Transparent

Is this nizamoffite?

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 nizamoffite with a known reference. Nizamoffite sits at Mohs ~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.
  • 4
    Match the color range
    Compare against the expected color range: colorless.
  • 5
    Look at form & habit
    Crystal system: orthorhombic. Typical habit: equant crystals.

Often confused with

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

Often found alongside nizamoffite

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

All properties

Chemical formula
MnZn₂(PO₄)₂(H₂O)₄
Mohs hardness
~3.5
Density
3.00 g/cm³
Colors
Streak
White
Luster
Vitreous
Transparency
Transparent
Crystal system
Orthorhombic
Crystal habit
Equant crystals
Cleavage
Perfect on {010}, good on {100}, and fair on {001}
Rarity
Rare
Uses
Collector
Host rock
A relatively late-formed phase from secondary alteration of primary triphylite and associated sphalerite in the core margin of a granitic pegmatite

Where rockhounds find nizamoffite

Classic worldwide localities

  • Palermo No.1 pegmatite, North Groton, Grafton County, New Hampshire, USA

Field-hunting tip

Where it forms: A relatively late-formed phase from secondary alteration of primary triphylite and associated sphalerite in the core margin of a granitic pegmatite. If you start seeing childrenite-eosphorite, crandallite-goyazite, fairfieldite-messelite in float, you are in the right ground. Typical habit: equant crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify nizamoffite?+
Mohs hardness is ~3.5. Luster: vitreous. The streak is white. Common colors include colorless.
Where is nizamoffite found?+
Notable localities include Palermo No.1 pegmatite, North Groton, Grafton County, New Hampshire, USA.
What rocks look like nizamoffite?+
Nizamoffite is most often confused with Childrenite, Eosphorite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with nizamoffite?+
Nizamoffite commonly co-occurs with Childrenite-eosphorite, Crandallite-goyazite, Fairfieldite-messelite, Falsterite, Fluorapatite, Frondelite-rockbridgeite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does nizamoffite form in?+
Where it forms: A relatively late-formed phase from secondary alteration of primary triphylite and associated sphalerite in the core margin of a granitic pegmatite. Working float back to the host body is the standard way to chase a fresh occurrence.
What is nizamoffite used for?+
Nizamoffite is used in collector.

Find nizamoffite on the map

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