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 — that is 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.






