Fossilized ferns are preserved remains or impressions of prehistoric plants found primarily in carbonaceous shales and siltstones. Collectors look for high-contrast specimens where the organic carbon film has been preserved against a lighter or different colored sedimentary matrix.
Is this fossilized ferns?
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 fossilized ferns with a known reference. Fossilized Ferns sits at Mohs 3-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Fossilized Ferns leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Fossilized Ferns typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: black, brown, gray, tan.
- 5Look at form & habitTypical habit: imprint.
Often found alongside fossilized ferns
Minerals reported to co-occur with fossilized ferns. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 3-6
- Density
- 2.5-2.7 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal habit
- Imprint
- Cleavage
- None
- Rarity
- Common
- Uses
- Collector, Educational, Decorative
- Host rock
- Shale, Siltstone, Coal
- Typical price
- $5-50 for small specimens, $100+ for display-quality slabs
Where rockhounds find fossilized ferns
1 mapped spotsClassic worldwide localities
- Mazon Creek, USA
- Joggins, Canada
- Czech Republic
- Germany
- France
Field-hunting tip
Look in shale, siltstone, coal country — that is the host setting where fossilized ferns typically forms. If you start seeing pyrite, siderite, kaolinite in float, you are in the right ground. Field specimens usually show a imprint habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Oregon — start trip planning there.




