Claystone is a fine-grained, non-fissile sedimentary rock composed primarily of clay-sized particles. Unlike shale, it does not display fissility or splitting along thin parallel laminations and often feels smooth or powdery to the touch when dry.
Is this claystone?
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 claystone with a known reference. Claystone sits at Mohs 1-2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Claystone leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Claystone typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: gray, brown, red, yellow, black.
- 5Look at form & habitTypical habit: massive.
Often confused with
Claystone vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside claystone
Minerals reported to co-occur with claystone. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 1-2
- Density
- 2.0-2.6 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal habit
- Massive
- Cleavage
- None
- Rarity
- Common
- Uses
- Industrial, Geological Study
- Host rock
- Sedimentary Basins
- Typical price
- low, generally available as bulk specimen material
Where rockhounds find claystone
Classic worldwide localities
- worldwide
- Kentucky, USA
- London Basin, UK
- Paris Basin, France
Field-hunting tip
Look in sedimentary basins country, the host setting where claystone typically forms. If you start seeing quartz, feldspar, calcite 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.









