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.
Is this bigcreekite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch bigcreekite with a known reference. Bigcreekite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to pearly.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal 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.





