Levinsonite-(Y) is an extremely rare sulfate mineral often found as tiny, delicate bladed crystals or radial sprays. It is typically discovered in geological settings where weathering of sulfide minerals occurs in aluminum-rich environments.

Hardness
3
Mohs
Luster
Vitreous
Streak
White
Transparency
Transparent

Is this levinsonite-(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 levinsonite-(y) with a known reference. Levinsonite-(Y) sits at Mohs 3, 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: monoclinic. Typical habit: prismatic, water soluble.

Often confused with

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

Often found alongside levinsonite-(y)

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

All properties

Chemical formula
YAl(SO₄)₂((C₂)O₄)(H₂O)₄·8H₂O
Mohs hardness
3
Density
2.181 g/cm³
Colors
Streak
White
Luster
Vitreous
Transparency
Transparent
Crystal system
Monoclinic
Crystal habit
Prismatic, water soluble
Cleavage
On {101}, perfect
Rarity
Rare
Uses
Collector
Host rock
Formed by evaporative precipitation during weathering of pyritiferous phyllite, the rare earths probably derived from monazite and xenotime

Where rockhounds find levinsonite-(y)

Classic worldwide localities

  • Alum Cave Bluff, Great Smoky Mountains National Park, Tennessee, USA

Field-hunting tip

Where it forms: Formed by evaporative precipitation during weathering of pyritiferous phyllite, the rare earths probably derived from monazite and xenotime. If you start seeing zugshunstite-, epsomite, halotrichite in float, you are in the right ground. Typical habit: prismatic, water soluble. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify levinsonite-(y)?+
Mohs hardness is 3. Luster: vitreous. The streak is white. Common colors include colorless.
Where is levinsonite-(y) found?+
Notable localities include Alum Cave Bluff, Great Smoky Mountains National Park, Tennessee, USA.
What rocks look like levinsonite-(y)?+
Levinsonite-(Y) is most often confused with Alunite, Jarosite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with levinsonite-(y)?+
Levinsonite-(Y) commonly co-occurs with Zugshunstite-, Epsomite, Halotrichite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does levinsonite-(y) form in?+
Where it forms: Formed by evaporative precipitation during weathering of pyritiferous phyllite, the rare earths probably derived from monazite and xenotime. Working float back to the host body is the standard way to chase a fresh occurrence.
What is levinsonite-(y) used for?+
Levinsonite-(Y) is used in collector.

Find levinsonite-(y) on the map

RockHoundR shows mapped rockhounding spots, access rules, and lets you log every find.

Download on the App StoreGet it on Google Play