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 — that is 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.







