Howlite is a borate mineral most commonly found in massive, chalk-white nodules with dark gray veining that creates a spider-web pattern. Because it is porous, it is frequently dyed blue or green to imitate turquoise, often sold as 'Turquenite' or 'White Buffalo' stone.
Is this howlite?
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 howlite with a known reference. Howlite 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: subvitreous, glimmering.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: earthy, massive, nodular.
Often confused with
Howlite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside howlite
Minerals reported to co-occur with howlite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂B₅SiO₉(OH)₅
- Mohs hardness
- 3.5
- Density
- 2.53-2.59 g/cm³
- Streak
- White
- Luster
- Subvitreous, glimmering
- Transparency
- Translucent in thin fragments
- Crystal system
- Monoclinic
- Crystal habit
- Earthy, massive, nodular
- Cleavage
- None
- Fluorescence
- Bright sky blue under LW UV
- Rarity
- Common
- Uses
- Lapidary, Collector, Decorative
- Host rock
- In borate deposits
Where rockhounds find howlite
Classic worldwide localities
- Sterling Borax mine, Tick Canyon, near Lang, Los Angeles Co., California, USA
- Calico, San Bernardino Co., California, USA
- Gower Gulch and at the Billie mine, near Ryan, Inyo Co., California, USA
- Russell and other borate mines north of Lockwood Valley, Ventura Co., California, USA
- Windsor, Canada
- Wentworth, Canada
Field-hunting tip
Where it forms: In borate deposits. If you start seeing colemanite, ulexite, bakerite in float, you are in the right ground. Typical habit: earthy, massive, nodular. Train your eye for that shape before scanning the outcrop.



