Gibbsite is a primary mineral component of bauxite and typically appears in white, waxy, or pearly tabular crystals or botryoidal masses. It is commonly found in tropical weathering zones or as a secondary mineral in hydrothermal alteration environments.
Is this gibbsite?
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 gibbsite with a known reference. Gibbsite sits at Mohs 2.5-3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Gibbsite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Gibbsite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, grayish-white, yellowish, reddish-white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, massive, botryoidal, stalactitic.
Often confused with
Gibbsite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside gibbsite
Minerals reported to co-occur with gibbsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Al(OH)₃
- Mohs hardness
- 2.5-3.5
- Density
- 2.4 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Massive, Botryoidal, Stalactitic
- Cleavage
- Perfect Basal
- Rarity
- Common
- Uses
- Collector, Ore of Aluminum
- Host rock
- Bauxite Deposits, Hydrothermal Veins, Low-temperature Metamorphic Environments
- Typical price
- $10-50 thumbnail, $50-200 cabinet specimen
Where rockhounds find gibbsite
Classic worldwide localities
- Arkansas, USA
- Poços de Caldas, Brazil
- Les Baux-de-Provence, France
- Grythyttan, Sweden
- Suriname
Field-hunting tip
Look in bauxite deposits, hydrothermal veins, low-temperature metamorphic environments country — that is the host setting where gibbsite typically forms. If you start seeing boehmite, diaspore, goethite in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, botryoidal, stalactitic habit, so train your eye for that shape before scanning the outcrop.




