Mudstone is a fine-grained sedimentary rock formed from the compaction of silt and clay particles. Unlike shale, it lacks fissility, meaning it does not split into thin, parallel layers. It is ubiquitous in sedimentary sequences worldwide and often serves as a source rock for hydrocarbons.
Is this mudstone?
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 mudstone with a known reference. Mudstone sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Mudstone leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Mudstone typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: gray, brown, red, black.
- 5Look at form & habitTypical habit: massive.
Often confused with
Mudstone vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside mudstone
Minerals reported to co-occur with mudstone. 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
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal habit
- Massive
- Cleavage
- None
- Rarity
- Common
- Uses
- Industrial, Construction, Architectural
- Host rock
- Sedimentary Basins
- Typical price
- $1-10 for specimen
Where rockhounds find mudstone
Classic worldwide localities
- global
- United States
- United Kingdom
- China
- Germany
Field-hunting tip
Look in sedimentary basins country — that is the host setting where mudstone typically forms. If you start seeing quartz, clay minerals, 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.






