Grantsite is an extremely rare hydrated sodium-uranium-vanadium mineral primarily found in the uranium-bearing sandstones of the Colorado Plateau. It usually appears as massive, earthy, yellow-colored crusts or coatings, making it difficult to distinguish visually from associated minerals like tyuyamunite without X-ray diffraction analysis.
Is this grantsite?
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 grantsite with a known reference. Grantsite sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Grantsite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Grantsite typically shows a earthy luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-orange, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: massive.
Often confused with
Grantsite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside grantsite
Minerals reported to co-occur with grantsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₄(V,U)₄O₁₂·10H₂O
- Mohs hardness
- 2-3
- Density
- 3.5-4 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Earthy
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Sandstone
- Typical price
- $20-150 for small specimens
Where rockhounds find grantsite
Classic worldwide localities
- Grants district, New Mexico, USA
- Colorado Plateau, USA
Field-hunting tip
Look in sandstone country — that is the host setting where grantsite typically forms. If you start seeing tyuyamunite, gypsum, calcite in float, you are in the right ground. Field specimens usually show a massive habit, so train your eye for that shape before scanning the outcrop.




