Coal is a combustible sedimentary rock formed from ancient plant matter that has been buried and subjected to heat and pressure over millions of years. It varies significantly in quality and carbon content, ranging from soft brown lignite to hard, shiny anthracite. Collectors typically look for specimens showing clear plant impressions or distinct layering.

Hardness
0.5-2.5
Mohs
Luster
Dull to submetallic
Transparency
Opaque

Is this coal?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch coal with a known reference. Coal sits at Mohs 0.5-2.5, softer than the next harder reference, harder than the previous one.
  • 2
    Read the texture
    Look at a fresh break with a hand lens. Texture: Forms layers (seams); bituminous coal often banded bright and dull.
  • 3
    Pick out the minerals
    Composition: Carbon-rich rock from plant material; bituminous coal is about 84 percent carbon. Identify the two or three most abundant grains.
  • 4
    Read the luster
    Hold the specimen under a strong light. Luster: dull to submetallic.
  • 5
    Match the color range
    Compare against the expected color range: black, brown.

Often confused with

Coal vs. its common look-alikes, and how to tell them apart in the field.

Often found alongside coal

Minerals reported to co-occur with coal. Spotting these in float or country rock is a strong cue you are in the right ground.

All properties

Mohs hardness
0.5-2.5
Density
1.1-1.5 g/cm³
Luster
Dull to submetallic
Transparency
Opaque
Rarity
Common
Uses
Industrial, Fuel, Collector
Host rock
sedimentary coal seams
Texture
Forms layers (seams); bituminous coal often banded bright and dull
Composition
Carbon-rich rock from plant material; bituminous coal is about 84 percent carbon

Where rockhounds find coal

1 mapped spots

Classic worldwide localities

  • USA
  • China
  • Australia
  • India
  • Germany

Field-hunting tip

Where it forms: sedimentary coal seams. If you start seeing pyrite, siderite, kaolinite in float, you are in the right ground. In the U.S., the densest reported localities are in Montana. Start trip planning there.

Common questions

How do you identify coal?+
Mohs hardness is 0.5-2.5. Texture: Forms layers (seams); bituminous coal often banded bright and dull. Composition: Carbon-rich rock from plant material; bituminous coal is about 84 percent carbon. Luster: dull to submetallic. Common colors include black, brown.
Where is coal found?+
Notable localities include USA; China; Australia; India; Germany.
Can I find coal in the United States?+
RockHoundR maps 1 coal rockhounding spots across 1 U.S. states. The top states are Montana.
What rocks look like coal?+
Coal is most often confused with Jet. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with coal?+
Coal commonly co-occurs with Pyrite, Siderite, Kaolinite, Calcite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does coal form in?+
Where it forms: sedimentary coal seams. Working float back to the host body is the standard way to chase a fresh occurrence.
What is coal used for?+
Coal is used in industrial, fuel, collector.

Find coal on the map

RockHoundR shows mapped rockhounding spots, access rules, and lets you log every find.

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