Meta-aluminite is a rare secondary sulfate mineral formed by the dehydration of aluminite. It typically appears as dull, white earthy masses or crusts within clay deposits and is primarily sought after by advanced collectors of rare sulfate minerals.

Hardness
1-2
Mohs
Luster
Somewhat silky
Streak
White
Transparency
Semitransparent

Is this meta-aluminite?

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 meta-aluminite with a known reference. Meta-aluminite sits at Mohs 1-2, 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: somewhat silky.
  • 4
    Match the color range
    Compare against the expected color range: snow white.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: aggregates, nodular.

Often confused with

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

Often found alongside meta-aluminite

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

All properties

Chemical formula
Al₂SO₄(OH)₄·5H₂O
Mohs hardness
1-2
Density
2.18 g/cm³
Streak
White
Luster
Somewhat silky
Transparency
Semitransparent
Crystal system
Monoclinic
Crystal habit
Aggregates, nodular
Cleavage
None observed
Rarity
Rare
Uses
Collector
Host rock
A rare secondary mineral formed by reaction of acid sulfate solutions from oxidizing pyrite reacting with clay minerals (Fuemrole mine, Utah, USA)

Where rockhounds find meta-aluminite

Classic worldwide localities

  • Fuemrole mine, Temple Mountain, Emery Co., Utah, USA
  • Newhaven, Sussex, England

Field-hunting tip

Where it forms: A rare secondary mineral formed by reaction of acid sulfate solutions from oxidizing pyrite reacting with clay minerals (Fuemrole mine, Utah, USA). If you start seeing gypsum, basaluminite in float, you are in the right ground. Typical habit: aggregates, nodular. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify meta-aluminite?+
Mohs hardness is 1-2. Luster: somewhat silky. The streak is white. Common colors include snow white.
Where is meta-aluminite found?+
Notable localities include Fuemrole mine, Temple Mountain, Emery Co., Utah, USA; Newhaven, Sussex, England.
What rocks look like meta-aluminite?+
Meta-aluminite is most often confused with Aluminite, Gibbsite, Kaolinite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with meta-aluminite?+
Meta-aluminite commonly co-occurs with Gypsum, Basaluminite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does meta-aluminite form in?+
Where it forms: A rare secondary mineral formed by reaction of acid sulfate solutions from oxidizing pyrite reacting with clay minerals (Fuemrole mine, Utah, USA). Working float back to the host body is the standard way to chase a fresh occurrence.
What is meta-aluminite used for?+
Meta-aluminite is used in collector.

Find meta-aluminite on the map

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