Greywacke is a texturally immature, poorly sorted sandstone characterized by its dark color and high proportion of lithic fragments and rock grains. Collectors often find it in mountainous regions where deep-water marine sequences have been tectonically uplifted and exposed. It is easily identified by its gritty feel and lack of distinct bedding compared to typical sedimentary rocks.
Is this greywacke?
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 greywacke with a known reference. Greywacke sits at Mohs 6-7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Greywacke leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Greywacke typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: gray, dark gray, brownish gray.
- 5Look at form & habitTypical habit: massive.
Often confused with
Greywacke vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside greywacke
Minerals reported to co-occur with greywacke. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 6-7
- Density
- 2.6-2.7 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal habit
- Massive
- Cleavage
- None
- Rarity
- Common
- Uses
- Construction Aggregate, Decorative Stone, Educational
- Host rock
- Marine Sedimentary Basins
- Typical price
- $1-10 per specimen
Where rockhounds find greywacke
Classic worldwide localities
- New Zealand
- Scotland
- Wales
- California, USA
Field-hunting tip
Look in marine sedimentary basins country, the host setting where greywacke typically forms. If you start seeing quartz, feldspar, mica 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.






