Rock Identifier
Silicified Snail Fossil (Gastropod (likely replaced by Chalcedony/Quartz - SiO2)) — fossil
fossil

Silicified Snail Fossil

Gastropod (likely replaced by Chalcedony/Quartz - SiO2)

Hardness: 6.5-7 (Mohs scale), Color: Creamy white to pale yellow, Luster: Dull to waxy, Crystal Structure: Microcrystalline (Cryptocrystalline), Cleavage: None/Conchoidal fracture

Hardness
6
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Physical properties

Hardness: 6.5-7 (Mohs scale), Color: Creamy white to pale yellow, Luster: Dull to waxy, Crystal Structure: Microcrystalline (Cryptocrystalline), Cleavage: None/Conchoidal fracture

Formation & geological history

Formed through permineralization or replacement where silica-rich groundwater fills the voids of a buried shell or replaces the calcium carbonate structure over millions of years, often in sedimentary environments.

Uses & applications

Used primarily as decorative items, educational specimens for paleontological study, and as items for amateur fossil collecting.

Geological facts

This specimen shows 'Beekite' rings—white, orbicular concentric deposits of chalcedony that often form on the surface of silicified fossils. They are a classic marker of silica replacement in sedimentary rocks.

Field identification & locations

Identify by looking for the preservation of spiral biological forms (gastropoda) combined with the hardness of quartz (it will scratch glass). Commonly found in limestone or chert-rich sedimentary beds.