A fossilized fern is the preserved remains or impression of a prehistoric plant, found primarily in carbonaceous shale and siltstone. Collectors look for a high-contrast specimen where the organic carbon film has been preserved against a lighter or differently colored sedimentary matrix.
Is this fossilized fern?
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 fern with a known reference. Fossilized Fern 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 Fern leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Fossilized Fern 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 fern
Minerals reported to co-occur with fossilized fern. 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
Where rockhounds find fossilized fern
1 mapped spotsClassic worldwide localities
- Mazon Creek, USA
- Joggins, Canada
- Czech Republic
- Germany
- France
Field-hunting tip
Look in shale, siltstone, coal country, the host setting where fossilized fern 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.






