Clintonite is a brittle mica found primarily in contact-metamorphosed limestones and skarns. It typically forms tabular, six-sided crystals that appear more rigid and less flexible than other common micas.

Hardness
3.5-6
Mohs
Luster
Vitreous, pearly, submetallic
Streak
White, slightly yellow-gray
Transparency
Transparent to translucent

Is this clintonite?

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 clintonite with a known reference. Clintonite sits at Mohs 3.5-6, 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, slightly yellow-gray.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous, pearly, submetallic.
  • 4
    Match the color range
    Compare against the expected color range: colorless, green, yellow, red, reddish brown.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: massive, radial.

Often confused with

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

Often found alongside clintonite

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

All properties

Chemical formula
Ca(Mg,Al)₃(Al₃Si)O₁₀(OH)₂
Mohs hardness
3.5-6
Density
3.0-3.1 g/cm³
Streak
White, slightly yellow-gray
Luster
Vitreous, pearly, submetallic
Transparency
Transparent to translucent
Crystal system
Monoclinic
Crystal habit
Massive, radial
Cleavage
{001}, perfect
Rarity
Uncommon
Uses
Collector
Host rock
In chlorite schists; in metasomatically altered limestones; in siliceous skarns near contact metamorphic zones

Where rockhounds find clintonite

Classic worldwide localities

  • Amity, Edenville, and Warwick, Orange Co., New York, USA
  • Crestmore, Riverside Co., California, USA
  • Ludwig, Lyon Co., Nevada, USA
  • Sulzer, Prince of Wales Island, Alaska, USA
  • Mt. Monzoni and at Mts. Castone and Adamello, Trentino-Alto Adige, Italy
  • Pargas district, Finland

Field-hunting tip

Where it forms: In chlorite schists; in metasomatically altered limestones; in siliceous skarns near contact metamorphic zones. If you start seeing talc, spinel, grossular in float, you are in the right ground. Typical habit: massive, radial. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify clintonite?+
Mohs hardness is 3.5-6. Luster: vitreous, pearly, submetallic. The streak is white, slightly yellow-gray. Common colors include colorless, green, yellow, red.
Where is clintonite found?+
Notable localities include Amity, Edenville, and Warwick, Orange Co., New York, USA; Crestmore, Riverside Co., California, USA; Ludwig, Lyon Co., Nevada, USA; Sulzer, Prince of Wales Island, Alaska, USA; Mt. Monzoni and at Mts. Castone and Adamello, Trentino-Alto Adige, Italy.
What rocks look like clintonite?+
Clintonite is most often confused with Biotite, Muscovite, Phlogopite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with clintonite?+
Clintonite commonly co-occurs with Talc, Spinel, Grossular, Vesuvianite, Clinopyroxene, Monticellite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does clintonite form in?+
Where it forms: In chlorite schists; in metasomatically altered limestones; in siliceous skarns near contact metamorphic zones. Working float back to the host body is the standard way to chase a fresh occurrence.
What is clintonite used for?+
Clintonite is used in collector.

Find clintonite on the map

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