Wardsmithite is a very rare hydrated magnesium calcium borate mineral discovered in the borate deposits of California. It typically occurs as small, clear, dodecahedral crystals associated with other borate minerals in evaporite beds. Due to its scarcity and solubility, it is strictly a specimen for advanced mineral collectors.
Is this wardsmithite?
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 wardsmithite with a known reference. Wardsmithite sits at Mohs 2.5, 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.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: microscopic crystals, nodular.
Often confused with
Wardsmithite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside wardsmithite
Minerals reported to co-occur with wardsmithite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₅Mg(B₄O₇)₆·30H₂O
- Mohs hardness
- 2.5
- Density
- 1.85-1.88 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Microscopic crystals, nodular
- Cleavage
- {001}, good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare weathering product of priceite and colemanite
Where rockhounds find wardsmithite
Classic worldwide localities
- Hard Scramble claim, Black Mountains, 3 km north-northwest of Ryan, and on the Oliver Consolidated claim, 3 km west of Ryan, Death Valley, Inyo Co., California, USA
Field-hunting tip
Where it forms: A rare weathering product of priceite and colemanite. If you start seeing gowerite, ulexite, nobleite in float, you are in the right ground. Typical habit: microscopic crystals, nodular. Train your eye for that shape before scanning the outcrop.






