Teruggite is a rare calcium magnesium arsenate borate mineral typically found as small, delicate, colorless to white bladed crystals. It is primarily encountered in boron-rich evaporite deposits where it forms in association with other borate minerals. Due to its scarcity and arsenic content, it is primarily sought after by advanced mineral collectors.
Is this teruggite?
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 teruggite with a known reference. Teruggite 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.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: bladed crystals, radial aggregates.
Often confused with
Teruggite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside teruggite
Minerals reported to co-occur with teruggite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₄Mg[AsB₆O₁₁(OH)₆]₂·14H₂O
- Mohs hardness
- 2.5
- Density
- 2.149-2.20 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Bladed crystals, radial aggregates
- Cleavage
- On {001}, good; on {110}, fair
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In lacustrine borate deposits, typically associated with volcanic hot springs and diagensis of playa sediments
Where rockhounds find teruggite
Classic worldwide localities
- Loma Blanca borate deposit, eight km southwest of Coranzulí, Jujuy Province, Argentina
- Hisarcık borate mine, near Emet, Kütahya Province
Field-hunting tip
Where it forms: In lacustrine borate deposits, typically associated with volcanic hot springs and diagensis of playa sediments. If you start seeing inyoite, calcite, ulexite in float, you are in the right ground. Typical habit: bladed crystals, radial aggregates. Train your eye for that shape before scanning the outcrop.








