Vermiculite is a hydrated magnesium aluminum iron silicate mineral that forms through the alteration of phlogopite or biotite. It is well-known for its ability to expand significantly when heated, a property that makes it useful in gardening and industrial insulation, though collectors primarily seek it for its distinctive platy, micaceous crystal habits.

Hardness
1.5-2
Mohs
Luster
Pearly
Streak
White
Transparency
Translucent

Is this vermiculite?

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 vermiculite with a known reference. Vermiculite sits at Mohs 1.5-2 — softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Vermiculite leaves a white streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Vermiculite typically shows a pearly luster.
  • 4
    Match the color range
    Compare against the expected color range: brown, yellow-brown, golden-yellow, greenish.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: lamellar, micaceous, massive, platy.

Often confused with

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

Often found alongside vermiculite

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

All properties

Chemical formula
(Mg,Fe,Al)₃(Al,Si)₄O₁₀(OH)₂·4H₂O
Mohs hardness
1.5-2
Density
2.3-2.7 g/cm³
Streak
White
Luster
Pearly
Transparency
Translucent
Crystal system
Monoclinic
Crystal habit
Lamellar, Micaceous, Massive, Platy
Cleavage
Perfect Basal
Rarity
Common
Uses
Industrial, Horticultural, Insulation
Host rock
Ultramafic Rocks, Hydrothermal Deposits
Typical price
$5-30 for specimen-grade pieces

Where rockhounds find vermiculite

4 mapped spots

Classic worldwide localities

  • USA
  • South Africa
  • Brazil
  • China
  • Russia

Field-hunting tip

Look in ultramafic rocks, hydrothermal deposits country — that is the host setting where vermiculite typically forms. If you start seeing phlogopite, apatite, serpentine in float, you are in the right ground. Field specimens usually show a lamellar, micaceous, massive, platy habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in North Carolina, Georgia, Montana — start trip planning there.

Common questions

How do you identify vermiculite?+
Mohs hardness is 1.5-2. It typically shows a pearly luster. The streak is white. Common colors include brown, yellow-brown, golden-yellow, greenish.
Where is vermiculite found?+
Notable localities include USA; South Africa; Brazil; China; Russia.
Can I find vermiculite in the United States?+
RockHoundR maps 4 vermiculite rockhounding spots across 3 U.S. states — the top states are North Carolina, Georgia, Montana.
How much is vermiculite worth?+
Typical asking prices fall in the range of $5-30 for specimen-grade pieces. Quality, size, and provenance can move individual specimens well outside that range.
What rocks look like vermiculite?+
Vermiculite is most often confused with Biotite, Phlogopite, Chlorite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with vermiculite?+
Vermiculite commonly co-occurs with Phlogopite, Apatite, Serpentine, Magnetite, Corundum. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does vermiculite form in?+
Vermiculite typically forms in ultramafic rocks, hydrothermal deposits. Working float back to the host body is the standard way to chase a fresh occurrence.
What is vermiculite used for?+
Vermiculite is used in industrial, horticultural, insulation.

Find vermiculite on the map

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

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