Orthojoaquinite-(La) is an exceptionally rare member of the joaquinite group, primarily found in the gem-rich hydrothermal veins of the Idria mining district in California. It typically forms small, brownish-yellow tabular crystals associated with benitoite and neptunite. Collectors prize it for its unique chemistry and strictly limited type locality.
Is this orthojoaquinite-(la)?
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 orthojoaquinite-(la) with a known reference. Orthojoaquinite-(La) 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. Orthojoaquinite-(La) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Orthojoaquinite-(La) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, orange-brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals.
Often confused with
Orthojoaquinite-(La) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside orthojoaquinite-(la)
Minerals reported to co-occur with orthojoaquinite-(la). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaBa₂LaFeTi₂Si₈O₂₆(OH)·H₂O
- Mohs hardness
- 5-5.5
- Density
- 3.8-3.9 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Glaucophane Schist Inclusions in Serpentinite
- Typical price
- $100-500 thumbnail
Where rockhounds find orthojoaquinite-(la)
Classic worldwide localities
- San Benito County, California, USA
Field-hunting tip
Look in glaucophane schist inclusions in serpentinite country — that is the host setting where orthojoaquinite-(la) typically forms. If you start seeing benitoite, neptunite, serandite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.





