Stringhamite is a rare calcium copper silicate typically found as small, bright blue to blue-green tabular crystals. It is most famous for its occurrences in Utah, where it forms in cavities within skarn deposits and hydrothermal veins. Collectors prize it for its vibrant color and distinct crystal morphology.

Hardness
3
Mohs
Luster
Vitreous
Streak
Light blue
Transparency
Transparent to translucent

Is this stringhamite?

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 stringhamite with a known reference. Stringhamite 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: light blue.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: azure, blue violet, dark blue.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: aggregates.

Often confused with

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

Often found alongside stringhamite

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

All properties

Chemical formula
CaCuSiO₄·H₂O
Mohs hardness
3
Density
3.16-3.18 g/cm³
Colors
AzureBlue violetDark blue
Streak
Light blue
Luster
Vitreous
Transparency
Transparent to translucent
Crystal system
Monoclinic
Crystal habit
Aggregates
Cleavage
Good on {001}; imperfect on {100}
Rarity
Rare
Uses
Collector
Host rock
A retrograde reaction product between copper-bearing solutions and diopside in diopside-magnetite tactites (Bawana mine, Utah, USA)

Where rockhounds find stringhamite

Classic worldwide localities

  • Bawana mine, about six km northwest of Milford, Beaver Co., Utah, USA
  • Crestmore, Riverside Co., California, USA
  • Christmas copper mine, Gila Co., Arizona, USA
  • El Bronce mine, Tierra Amarilla, Copiapó, Chile

Field-hunting tip

Where it forms: A retrograde reaction product between copper-bearing solutions and diopside in diopside-magnetite tactites (Bawana mine, Utah, USA). If you start seeing thaumasite, tenorite, kinoite in float, you are in the right ground. Typical habit: aggregates. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify stringhamite?+
Mohs hardness is 3. Luster: vitreous. The streak is light blue. Common colors include azure, blue violet, dark blue.
Where is stringhamite found?+
Notable localities include Bawana mine, about six km northwest of Milford, Beaver Co., Utah, USA; Crestmore, Riverside Co., California, USA; Christmas copper mine, Gila Co., Arizona, USA; El Bronce mine, Tierra Amarilla, Copiapó, Chile.
Is stringhamite safe to handle?+
Stringhamite contains copper. Wash your hands afterwards, never grind or breathe the dust, and store it apart from specimens you handle often.
What rocks look like stringhamite?+
Stringhamite is most often confused with Ajoite, Chrysocolla. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with stringhamite?+
Stringhamite commonly co-occurs with Thaumasite, Tenorite, Kinoite, Calcite, Apophyllite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does stringhamite form in?+
Where it forms: A retrograde reaction product between copper-bearing solutions and diopside in diopside-magnetite tactites (Bawana mine, Utah, USA). Working float back to the host body is the standard way to chase a fresh occurrence.
What is stringhamite used for?+
Stringhamite is used in collector.

Find stringhamite on the map

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