Esquireite is a rare barium silicate mineral primarily known from the Big Creek mining district in California. It typically occurs as colorless to white thin, platy crystals associated with sanbornite in metamorphic assemblages.

Hardness
~2
Mohs
Luster
Vitreous to pearly
Streak
White
Transparency
Transparent

Is this esquireite?

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 esquireite with a known reference. Esquireite sits at Mohs ~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: vitreous to pearly.
  • 4
    Match the color range
    Compare against the expected color range: colorless.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: platy crystals.

Often confused with

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

Often found alongside esquireite

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

All properties

Chemical formula
BaSi₆O₁₃·7H₂O
Mohs hardness
~2
Density
2.18 g/cm³
Colors
Streak
White
Luster
Vitreous to pearly
Transparency
Transparent
Crystal system
Monoclinic
Crystal habit
Platy crystals
Cleavage
Perfect on {001}, fair on {100}
Rarity
Rare
Uses
Collector
Host rock
Formed by low-temperature hydrothermal alteration of sanbornite, during contact metamorphism of Ba-rich sediments

Where rockhounds find esquireite

Classic worldwide localities

  • Esquire #1 claim, near Rush Creek and the Esquire #8 claim, on Big Creek, eastern Fresno County and on the NW slope of Trumbull Peak, Mariposa County, California, USA

Field-hunting tip

Where it forms: Formed by low-temperature hydrothermal alteration of sanbornite, during contact metamorphism of Ba-rich sediments. If you start seeing cerchiaraite-, kampfite, macdonaldite in float, you are in the right ground. Typical habit: platy crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify esquireite?+
Mohs hardness is ~2. Luster: vitreous to pearly. The streak is white. Common colors include colorless.
Where is esquireite found?+
Notable localities include Esquire #1 claim, near Rush Creek and the Esquire #8 claim, on Big Creek, eastern Fresno County and on the NW slope of Trumbull Peak, Mariposa County, California, USA.
What rocks look like esquireite?+
Esquireite is most often confused with Sanbornite, Celsian. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with esquireite?+
Esquireite commonly co-occurs with Cerchiaraite-, Kampfite, Macdonaldite, Pyrrhotite, Quartz, Titantaramellite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does esquireite form in?+
Where it forms: Formed by low-temperature hydrothermal alteration of sanbornite, during contact metamorphism of Ba-rich sediments. Working float back to the host body is the standard way to chase a fresh occurrence.
What is esquireite used for?+
Esquireite is used in collector.

Find esquireite on the map

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