Picasso stone is a trade name for metamorphosed limestone from the Mineral Mountains of southwestern Utah, mostly in Beaver County. Heat, pressure and fluids linked to Tertiary igneous intrusions recrystallized the limestone into marble and filled a network of fractures with dark minerals such as graphite and iron oxides, giving black, gray, tan and cream patterns. It is also sold as Picasso marble, Painter's Marble and Picasso jasper, although it is not a jasper.
Is this picasso stone?
3-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Read the textureLook at a fresh break with a hand lens. Texture: Marble cut by a network of fractures filled with dark minerals.
- 2Pick out the mineralsComposition: Recrystallized limestone (marble) with graphite, hematite and iron oxides in fractures. Identify the two or three most abundant grains.
- 3Match the color rangeCompare against the expected color range: black, gray, tan, cream.
Often confused with
Picasso Stone vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside picasso stone
Minerals reported to co-occur with picasso stone. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Uses
- Decorative
- Host rock
- Metamorphosed limestone of the Mineral Mountains, southwestern Utah
- Texture
- Marble cut by a network of fractures filled with dark minerals
- Composition
- Recrystallized limestone (marble) with graphite, hematite and iron oxides in fractures
Where rockhounds find picasso stone
Classic worldwide localities
- Mineral Mountains, Beaver County, Utah
Field-hunting tip
Where it forms: Metamorphosed limestone of the Mineral Mountains, southwestern Utah. If you start seeing graphite, hematite in float, you are in the right ground.



