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, 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.







