Shale is a fine-grained sedimentary rock formed from the compaction of silt and clay-sized mineral particles. It is defined by its characteristic fissility, allowing it to split into thin, parallel layers along bedding planes. It is the most abundant sedimentary rock on Earth and frequently contains fossils or organic material.

Hardness
2-3
Mohs
Luster
Dull
Transparency
Opaque

Is this shale?

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 shale with a known reference. Shale sits at Mohs 2-3, 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: Fissile; splits into thin layers under 1 cm thick. Grain size: Fine-grained (particles under 0.0625 mm).
  • 3
    Pick out the minerals
    Composition: Clay mineral flakes with silt-sized fragments of other minerals, especially quartz and calcite. Identify the two or three most abundant grains.
  • 4
    Read the luster
    Hold the specimen under a strong light. Luster: dull.
  • 5
    Match the color range
    Compare against the expected color range: gray, black, red, brown, green.

Often confused with

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

Often found alongside shale

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

All properties

Mohs hardness
2-3
Density
2.0-2.6 g/cm³
Luster
Dull
Transparency
Opaque
Rarity
Common
Uses
Industrial, Construction, Collector
Host rock
sedimentary basins
Texture
Fissile; splits into thin layers under 1 cm thick
Grain size
Fine-grained (particles under 0.0625 mm)
Composition
Clay mineral flakes with silt-sized fragments of other minerals, especially quartz and calcite

Where rockhounds find shale

2 mapped spots

Classic worldwide localities

  • USA
  • China
  • Canada
  • Germany
  • United Kingdom

Field-hunting tip

Where it forms: sedimentary basins. If you start seeing quartz, clay minerals, calcite in float, you are in the right ground. In the U.S., the densest reported localities are in Montana, New Jersey. Start trip planning there.

Common questions

How do you identify shale?+
Mohs hardness is 2-3. Texture: Fissile; splits into thin layers under 1 cm thick. Composition: Clay mineral flakes with silt-sized fragments of other minerals, especially quartz and calcite. Luster: dull. Common colors include gray, black, red, brown.
Where is shale found?+
Notable localities include USA; China; Canada; Germany; United Kingdom.
Can I find shale in the United States?+
RockHoundR maps 2 shale rockhounding spots across 2 U.S. states. The top states are Montana, New Jersey.
What rocks look like shale?+
Shale is most often confused with Slate, Siltstone, Mudstone. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with shale?+
Shale commonly co-occurs with Quartz, Clay minerals, Calcite, Pyrite, Feldspar. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does shale form in?+
Where it forms: sedimentary basins. Working float back to the host body is the standard way to chase a fresh occurrence.
What is shale used for?+
Shale is used in industrial, construction, collector.

Find shale on the map

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

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