Paraniite-(Y) is a rare calcium yttrium arsenate that forms creamy yellow rough crystals. It was approved as a distinct mineral species in 1992. It was first described from the east flank of Pizzo Cervandone, Alpe Devero, Valle d'Ossola, Piedmont, Italy.

Hardness
3-4
Mohs
Luster
Vitreous to adamantine
Streak
Yellowish-white
Transparency
Semitransparent

Is this paraniite-(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 paraniite-(y) with a known reference. Paraniite-(Y) sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: yellowish-white.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous to adamantine.
  • 4
    Match the color range
    Compare against the expected color range: yellow.
  • 5
    Look at form & habit
    Crystal system: tetragonal. Typical habit: rough crystals.

Often confused with

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

Often found alongside paraniite-(y)

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

All properties

Chemical formula
Ca₂Y(WO₄)₂(AsO₄)
Mohs hardness
3-4
Density
5.95 g/cm³
Colors
Streak
Yellowish-white
Luster
Vitreous to adamantine
Transparency
Semitransparent
Crystal system
Tetragonal
Crystal habit
Rough crystals
Cleavage
On {001}, distinct
Rarity
Rare
Uses
Collector
Host rock
A very rare mineral found in a fissure in gneiss in an area anomalously high in arsenic (Pizzo Cervandone, Italy)

Where rockhounds find paraniite-(y)

Classic worldwide localities

  • East flank of Pizzo Cervandone, Alpe Devero, Valle d’Ossola, Piedmont, Italy
  • Fianel mine, Val Ferrera, Graubünden, Switzerland

Field-hunting tip

Where it forms: A very rare mineral found in a fissure in gneiss in an area anomalously high in arsenic (Pizzo Cervandone, Italy). If you start seeing scheelite–powellite, beryl, roméite in float, you are in the right ground. Typical habit: rough crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify paraniite-(y)?+
Mohs hardness is 3-4. Luster: vitreous to adamantine. The streak is yellowish-white. Common colors include yellow.
Where is paraniite-(y) found?+
Notable localities include East flank of Pizzo Cervandone, Alpe Devero, Valle d’Ossola, Piedmont, Italy; Fianel mine, Val Ferrera, Graubünden, Switzerland.
Is paraniite-(y) safe to handle?+
Paraniite-(Y) contains arsenic and calls for real care. Contains arsenic, which is toxic if ingested or inhaled as dust. Wash hands thoroughly after handling and avoid creating dust.
What rocks look like paraniite-(y)?+
Paraniite-(Y) is most often confused with Tundrite-(Nd), Stillwellite-(Ce). A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with paraniite-(y)?+
Paraniite-(Y) commonly co-occurs with Scheelite–powellite, Beryl, Roméite, Betafite, Fluorapatite, Bergslagite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does paraniite-(y) form in?+
Where it forms: A very rare mineral found in a fissure in gneiss in an area anomalously high in arsenic (Pizzo Cervandone, Italy). Working float back to the host body is the standard way to chase a fresh occurrence.
What is paraniite-(y) used for?+
Paraniite-(Y) is used in collector.

Find paraniite-(y) on the map

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