Gilsonite is a naturally occurring solid hydrocarbon resin found in massive, brittle veins. It is known for its high luster and distinct brown streak, often appearing indistinguishable from obsidian or black glass to the untrained eye.
Is this gilsonite?
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 gilsonite with a known reference. Gilsonite sits at Mohs 2-2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Gilsonite leaves a brown streak.
- 3Read the lusterHold the specimen under a strong light. Gilsonite typically shows a bright luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitTypical habit: massive.
Often confused with
Gilsonite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside gilsonite
Minerals reported to co-occur with gilsonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 2-2.5
- Density
- 1.05-1.10 g/cm³
- Colors
- Streak
- Brown
- Luster
- Bright
- Transparency
- Opaque
- Crystal habit
- Massive
- Cleavage
- Conchoidal Fracture
- Rarity
- Common
- Uses
- Industrial, Collector
- Host rock
- Sedimentary Veins in Sandstone
- Typical price
- $5-30 specimen
Where rockhounds find gilsonite
1 mapped spotsClassic worldwide localities
- Uintah Basin, Utah, USA
- Duchesne County, Utah, USA
Field-hunting tip
Look in sedimentary veins in sandstone country — that is the host setting where gilsonite typically forms. If you start seeing calcite, quartz 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. In the U.S., the densest reported localities are in Utah — start trip planning there.




