Boggsite is an extremely rare zeolite mineral discovered in the basalt vesicles of Oregon. It typically forms small, clear, pseudo-dodecahedral crystals that are highly sought after by systematic mineral collectors.
Is this boggsite?
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 boggsite with a known reference. Boggsite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Boggsite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Boggsite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: equant pseudo-dodecahedral crystals.
Often confused with
Boggsite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside boggsite
Minerals reported to co-occur with boggsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₈Na₃(Si₄₈Be₂Al₄₈)O₉₆·70H₂O
- Mohs hardness
- 3.5
- Density
- 2.12 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Equant Pseudo-dodecahedral Crystals
- Cleavage
- None Observed
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Vesicles in Basalt
- Typical price
- $50-300 per specimen
Where rockhounds find boggsite
Classic worldwide localities
- Gobalou Lave, Goble, Oregon, USA
Field-hunting tip
Look in vesicles in basalt country — that is the host setting where boggsite typically forms. If you start seeing quartz, calcite, heulandite in float, you are in the right ground. Field specimens usually show a equant pseudo-dodecahedral crystals habit, so train your eye for that shape before scanning the outcrop.






