Bigcreekite is an extremely rare barium-calcium silicate mineral known almost exclusively from its type locality at the Big Creek drainage in California. It typically occurs as small, colorless, platy, or tabular crystals associated with other rare barium minerals in metamorphic rock environments.

Hardness
2-3
Mohs
Luster
Vitreous to pearly
Streak
White
Transparency
Translucent

Is this bigcreekite?

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 bigcreekite with a known reference. Bigcreekite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: 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, white.
  • 5
    Look at form & habit
    Crystal system: orthorhombic. Typical habit: subhedral crystals, tabular.

Often confused with

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

Often found alongside bigcreekite

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

All properties

Chemical formula
BaSi₂O₅·4H₂O
Mohs hardness
2-3
Density
2.66 g/cm³
Streak
White
Luster
Vitreous to pearly
Transparency
Translucent
Crystal system
Orthorhombic
Crystal habit
Subhedral crystals, tabular
Cleavage
Perfect on {001} and {010}
Rarity
Rare
Uses
Collector
Host rock
Filling fractures in gneiss near the margins of a granodiorite pluton

Where rockhounds find bigcreekite

Classic worldwide localities

  • Esquire #7 claim, west side of Big Creek, eastern Fresno County, and on the northwestern slope of Trumbull Peak, Mariposa County, California, USA

Field-hunting tip

Where it forms: Filling fractures in gneiss near the margins of a granodiorite pluton. If you start seeing sanbornite, quartz, diopside in float, you are in the right ground. Typical habit: subhedral crystals, tabular. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify bigcreekite?+
Mohs hardness is 2-3. Luster: vitreous to pearly. The streak is white. Common colors include colorless, white.
Where is bigcreekite found?+
Notable localities include Esquire #7 claim, west side of Big Creek, eastern Fresno County, and on the northwestern slope of Trumbull Peak, Mariposa County, California, USA.
What rocks look like bigcreekite?+
Bigcreekite is most often confused with Delrioite, Apophyllite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with bigcreekite?+
Bigcreekite commonly co-occurs with Sanbornite, Quartz, Diopside, Pyrrhotite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does bigcreekite form in?+
Where it forms: Filling fractures in gneiss near the margins of a granodiorite pluton. Working float back to the host body is the standard way to chase a fresh occurrence.
What is bigcreekite used for?+
Bigcreekite is used in collector.

Find bigcreekite on the map

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