Tabbyite is a variety of bitumen or asphaltum found primarily in the Uinta Basin of Utah. It is a solid, brittle hydrocarbon that presents as a dark brown to black mass with a distinct resinous luster and often exhibits conchoidal fracture.
Is this tabbyite?
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 tabbyite with a known reference. Tabbyite 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. Streak: brown.
- 3Read the lusterHold the specimen under a strong light. Luster: resinous.
- 4Match the color rangeCompare against the expected color range: black, brown.
- 5Look at form & habitTypical habit: massive.
Often confused with
Tabbyite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Luster reads resinous on Tabbyite and bright on Gilsonite.

How to tell apart: Tabbyite is noticeably harder (Mohs 2-3 vs. 1); streak differs, so Tabbyite leaves brown, Ozokerite leaves white to yellowish; luster reads resinous on Tabbyite and greasy on Ozokerite.
Often found alongside tabbyite
Minerals reported to co-occur with tabbyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 2-3
- Density
- 1.05-1.15 g/cm³
- Streak
- Brown
- Luster
- Resinous
- Transparency
- Opaque
- Crystal habit
- Massive
- Cleavage
- None
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- sedimentary
Where rockhounds find tabbyite
1 mapped spotsClassic worldwide localities
- Tabby Canyon, Utah, USA
- Uinta Basin, Utah, USA
Field-hunting tip
Where it forms: sedimentary. If you start seeing sandstone, shale in float, you are in the right ground. Typical habit: massive. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Utah. Start trip planning there.


