Siltstone is a fine-grained sedimentary rock composed mainly of silt-sized particles. It feels gritty to the touch compared to claystone or shale and is commonly found in river channels, deltas, and floodplains.
Is this siltstone?
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 siltstone with a known reference. Siltstone sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Siltstone leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Siltstone typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: gray, red, brown, tan, green.
- 5Look at form & habitTypical habit: massive.
Often confused with
Siltstone vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside siltstone
Minerals reported to co-occur with siltstone. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 3-4
- Density
- 2.2-2.6 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal habit
- Massive
- Cleavage
- None
- Rarity
- Common
- Uses
- Construction, Decorative, Educational
- Host rock
- Sedimentary Basins
- Typical price
- $1-10 per specimen
Where rockhounds find siltstone
Classic worldwide localities
- USA
- United Kingdom
- Germany
- China
- Australia
Field-hunting tip
Look in sedimentary basins country, the host setting where siltstone 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.






