Fossil Identification Guide

Found something and wondering what it is? Browse our visual identification guides for the most common fossil types found across the United States.

Ammonites fossil specimen

Ammonites

Devonian to Cretaceous (419-66 million years ago)

Extinct cephalopods with distinctive coiled shells and intricate suture patterns. Ammonites are among the most recognizable fossils in the world, found across the United States in marine sedimentary rocks from the Devonian through the end of the Cretaceous.

Coiled (planispiral) shellComplex suture patterns visible on weathered shellsCentral siphuncle (tube connecting chambers)
Brachiopods fossil specimen

Brachiopods

Cambrian to present (521-0 million years ago, mostly Paleozoic)

Marine animals with two-valved shells that superficially resemble clams but belong to an entirely different phylum. Brachiopods were dominant members of Paleozoic sea floors and are among the most common fossils found in the eastern and central United States.

Symmetry across each valve (not between valves like clams)Pedicle opening (hole or notch for attachment stalk)Two unequal-sized valves
Crinoids fossil specimen

Crinoids

Ordovician to present (485-0 million years ago)

Marine echinoderms commonly called sea lilies, related to starfish and sea urchins rather than plants. Crinoid stem segments are among the most abundant fossils in Paleozoic limestones across the American Midwest.

Round disc-shaped stem segments (columnals) with central holeCalyx (cup-shaped head) made of interlocking platesBranching arms (brachioles) for filter feeding

Dinosaur Bone

Triassic to Cretaceous (230-66 million years ago)

How to identify fossilized dinosaur bone, including the tongue test, cross-section texture, weight, color, and how to distinguish real bone from petrified wood, ironstone, and volcanic rock.

Spongy internal textureHeavy for its sizeSticks to tongue

Dinosaur Tracks

Triassic to Cretaceous (230-66 million years ago)

How to identify fossilized dinosaur tracks and trackways, including theropod, sauropod, and ornithopod prints, with guidance on distinguishing real tracks from natural erosion features.

Three-toed impressions (theropods)Round/oval prints (sauropods)Found in fine sandstone/mudstone
Petrified Wood fossil specimen

Petrified Wood

Various periods (most collected specimens are Triassic to Miocene, 252-5 million years ago)

Fossil wood in which the original organic material has been replaced by minerals, most commonly silica (quartz), preserving the tree's cellular structure in stone. Petrified wood is found across the western and southern United States and is one of the most visually striking fossils a collector can find.

Visible wood grain and growth rings preserved in stoneCellular structure visible under magnificationHeavy weight (quartz density, ~2.65 g/cm3)
Shark Teeth fossil specimen

Shark Teeth

Devonian to present (419-0 million years ago)

Fossilized teeth from sharks and their relatives, preserved because shark skeletons are cartilage but their teeth are made of durable enameloid and dentine. Shark teeth are among the most accessible and widely collected fossils in the United States.

Distinct crown (blade) and root structureEnameloid coating on crown (glossy, often dark)Serrations along blade edges in many species
Trilobites fossil specimen

Trilobites

Cambrian to Permian (521-252 million years ago)

Ancient marine arthropods with segmented bodies and compound eyes. Among the most popular fossils for collectors, found across many US states in rocks from Cambrian to Permian age.

Three-lobed body planSegmented thoraxCompound eyes