Bivalve fossils are the mineralized remains of mollusks, characterized by two matching hinged shells. They are frequently found in sedimentary layers and are often preserved as casts, molds, or replaced by silica or calcite through permineralization.
Is this bivalve fossil?
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 bivalve fossil with a known reference. Bivalve Fossil sits at Mohs 3-5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Bivalve Fossil leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Bivalve Fossil typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: tan, brown, gray, white, cream.
- 5Look at form & habitTypical habit: bivalved shells.
Often found alongside bivalve fossil
Minerals reported to co-occur with bivalve fossil. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 3-5
- Density
- 2.0-2.7 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal habit
- Bivalved Shells
- Cleavage
- None
- Rarity
- Common
- Uses
- Collector, Educational, Decorative
- Host rock
- Sedimentary Rock
- Typical price
- $5-50 depending on preservation and size
Where rockhounds find bivalve fossil
Classic worldwide localities
- United Kingdom
- United States
- Germany
- France
- Morocco
Field-hunting tip
Look in sedimentary rock country — that is the host setting where bivalve fossil typically forms. If you start seeing calcite, quartz, pyrite in float, you are in the right ground. Field specimens usually show a bivalved shells habit, so train your eye for that shape before scanning the outcrop.




