Clinojimthompsonite is a rare chain silicate mineral that forms as a structural variation of jimthompsonite. It is typically found in association with other magnesium silicates in altered ultramafic rocks and is often difficult to distinguish from its orthorhombic counterpart without X-ray diffraction analysis.

Hardness
2-2.5
Mohs
Luster
Silky to pearly
Streak
White
Transparency
Semitransparent

Is this clinojimthompsonite?

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 clinojimthompsonite with a known reference. Clinojimthompsonite sits at Mohs 2-2.5, 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: silky to pearly.
  • 4
    Match the color range
    Compare against the expected color range: colorless, pink brown.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: prismatic crystals.

Often confused with

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

Often found alongside clinojimthompsonite

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

All properties

Chemical formula
Mg₅Si₆O₁₆(OH)₂
Mohs hardness
2-2.5
Density
3.02 g/cm³
Streak
White
Luster
Silky to pearly
Transparency
Semitransparent
Crystal system
Monoclinic
Crystal habit
Prismatic crystals
Cleavage
{110} predicted from the structure
Rarity
Rare
Uses
Collector
Host rock
In the black wallrock between chlorite and actinolite zones of a metamorphosed ultramafic body

Where rockhounds find clinojimthompsonite

Classic worldwide localities

  • Carleton talc quarry, near Chester, Windsor Co., Vermont, USA

Field-hunting tip

Where it forms: In the black wallrock between chlorite and actinolite zones of a metamorphosed ultramafic body. If you start seeing chesterite, clinojimthompsonite, anthophyllite in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify clinojimthompsonite?+
Mohs hardness is 2-2.5. Luster: silky to pearly. The streak is white. Common colors include colorless, pink brown.
Where is clinojimthompsonite found?+
Notable localities include Carleton talc quarry, near Chester, Windsor Co., Vermont, USA.
What rocks look like clinojimthompsonite?+
Clinojimthompsonite is most often confused with Jimthompsonite, Anthophyllite, Talc. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with clinojimthompsonite?+
Clinojimthompsonite commonly co-occurs with Chesterite, Clinojimthompsonite, Anthophyllite, Cummingtonite, Talc. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does clinojimthompsonite form in?+
Where it forms: In the black wallrock between chlorite and actinolite zones of a metamorphosed ultramafic body. Working float back to the host body is the standard way to chase a fresh occurrence.
What is clinojimthompsonite used for?+
Clinojimthompsonite is used in collector.

Find clinojimthompsonite on the map

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