Brewsterite-Ba is a rare member of the zeolite group often found as small, glassy tabular crystals in basalt cavities. It is most easily identified by its distinct platy habit and strong association with other zeolites and secondary minerals in volcanic rocks.
Is this brewsterite-ba?
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 brewsterite-ba with a known reference. Brewsterite-Ba sits at Mohs 5-5.5, 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 on {010}.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale pink.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, radiating clusters.
Often confused with
Brewsterite-Ba vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside brewsterite-ba
Minerals reported to co-occur with brewsterite-ba. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ba(Al₂Si₆)O₁₆·5H₂O
- Mohs hardness
- 5-5.5
- Density
- 2.45 g/cm³
- Streak
- White
- Luster
- Vitreous to pearly on {010}
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular crystals, radiating clusters
- Cleavage
- {010}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermally deposited in druses lining cavities in basalts and schists; more rarely in ore deposits
Where rockhounds find brewsterite-ba
Classic worldwide localities
- Strontian, Argyllshire, Scotland
- Burpala massif, about 120 km north of Lake Baikal, eastern Siberia, Russia
- Yellow Lake, near Olalla, British Columbia, Canada
Field-hunting tip
Where it forms: Hydrothermally deposited in druses lining cavities in basalts and schists; more rarely in ore deposits. If you start seeing zeolites, calcite, quartz in float, you are in the right ground. Typical habit: tabular crystals, radiating clusters. Train your eye for that shape before scanning the outcrop.





