
sedimentary
Ammonite Fossil
Ammonoidea (subclass)
AI-generated identification · may be incorrectHardness: 3-4 (if calcified/pyritized); Color: brown, tan, or metallic if pyritized; Luster: earthy to pearly; Crystal structure: orthorhombic/hexagonal (aragonite/calcite replacement); coiled chambered shell with ribbing.
- Hardness
- 3-4 (if calcified/pyritized)
- Color
- brown, tan, or metallic if pyritized
- Luster
- earthy to pearly
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Physical properties
Hardness: 3-4 (if calcified/pyritized); Color: brown, tan, or metallic if pyritized; Luster: earthy to pearly; Crystal structure: orthorhombic/hexagonal (aragonite/calcite replacement); coiled chambered shell with ribbing.
Formation & geological history
Formed through the process of permineralization or replacement where mud and minerals fill the shell of a prehistoric cephalopod. These specimens date from the Devonian to the Cretaceous period (approx. 400 to 66 million years ago).
Uses & applications
Used primarily for paleontological study, jewelry (especially iridescent 'Ammolite'), home decor, and educational collections.
Geological facts
Ammonites are extinct marine mollusks related to modern squids and octopuses. Their name comes from the Egyptian god Ammon, who was often depicted with ram's horns which the fossils resemble.
Field identification & locations
Identify by its spiral shape and distinctive ribbing. Commonly found in sedimentary rock formations like shale or limestone. Collectors look for sutures (growth lines) or opal-like iridescence on the surface.
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