Fluorbritholite-(Y) is a rare rare-earth silicate mineral belonging to the apatite supergroup. It is typically found as small, prismatic, brownish to yellow crystals in alkaline pegmatite environments and is often slightly radioactive due to thorium or uranium substitutions.

Hardness
5.5
Mohs
Luster
Vitreous to greasy; resinous [metamict]
Streak
Pale brown to almost white
Transparency
Transparent

Is this fluorbritholite-(y)?

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 fluorbritholite-(y) with a known reference. Fluorbritholite-(Y) sits at Mohs 5.5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: pale brown to almost white.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous to greasy; resinous [metamict].
  • 4
    Match the color range
    Compare against the expected color range: brown-pink, dark brown.
  • 5
    Look at form & habit
    Crystal system: hexagonal. Typical habit: prismatic crystals, massive.

Often confused with

Fluorbritholite-(Y) vs. its common look-alikes, and how to tell them apart in the field.

Often found alongside fluorbritholite-(y)

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

All properties

Chemical formula
(Y,Ca)₅(SiO₄)₃F
Mohs hardness
5.5
Density
4.609 g/cm³
Colors
Brown-pinkDark brown
Streak
Pale brown to almost white
Luster
Vitreous to greasy; resinous [metamict]
Transparency
Transparent
Crystal system
Hexagonal
Crystal habit
Prismatic crystals, massive
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
In pegmatite cutting alkaline granite

Where rockhounds find fluorbritholite-(y)

Classic worldwide localities

  • Lagmannsvik and Kråkmo, Hamarøy, Nordland, Norway, and at Mt. Vyuntspakhk, Western Keivy, Kola Peninsula, Russia

Field-hunting tip

Where it forms: In pegmatite cutting alkaline granite. If you start seeing y-bearing fluorite, allanite-, quartz in float, you are in the right ground. Typical habit: prismatic crystals, massive. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify fluorbritholite-(y)?+
Mohs hardness is 5.5. Luster: vitreous to greasy; resinous [metamict]. The streak is pale brown to almost white. Common colors include brown-pink, dark brown.
Where is fluorbritholite-(y) found?+
Notable localities include Lagmannsvik and Kråkmo, Hamarøy, Nordland, Norway, and at Mt. Vyuntspakhk, Western Keivy, Kola Peninsula, Russia.
Is fluorbritholite-(y) safe to handle?+
Fluorbritholite-(Y) contains trace uranium or thorium. Contains minor rare earth elements and uranium/thorium impurities; handle with care and wash hands after handling to avoid ingestion of dust.
What rocks look like fluorbritholite-(y)?+
Fluorbritholite-(Y) is most often confused with Apatite, Britholite-(Ce), Steenstrupine-(Ce). A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with fluorbritholite-(y)?+
Fluorbritholite-(Y) commonly co-occurs with Y-bearing fluorite, Allanite-, Quartz, Aluminocerite-, Bastnäsite-, Britholite-. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does fluorbritholite-(y) form in?+
Where it forms: In pegmatite cutting alkaline granite. Working float back to the host body is the standard way to chase a fresh occurrence.
What is fluorbritholite-(y) used for?+
Fluorbritholite-(Y) is used in collector.

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