
sedimentary
Fossilized Angel Wing Shell
Cyrtopleura costata
Hardness: 2.5-3.5 (Mohs scale), Color: Creamy white to grayish-white, Luster: Dull or chalky, Structure: Fragile thinned shell with radiating ribs and tooth-like serrations, Mineral composition: Calcium carbonate (Calcite/Aragonite).
- Hardness
- 2
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Physical properties
Hardness: 2.5-3.5 (Mohs scale), Color: Creamy white to grayish-white, Luster: Dull or chalky, Structure: Fragile thinned shell with radiating ribs and tooth-like serrations, Mineral composition: Calcium carbonate (Calcite/Aragonite).
Formation & geological history
Formed through the process of permineralization or as a trace fossil preservation in marine sedimentary layers. Specifically found in Pliocene and Pleistocene deposits (approx. 10,000 to 5 million years old) where soft-bottom marine environments existed.
Uses & applications
Used primarily for educational study, paleontology collections, and as decorative coastal display pieces.
Geological facts
The Angel Wing clam is a piddock that burrows as deep as three feet into sand or mud. They are so named because the two valves of the shell together look like the wings of an angel. Unlike many other clams, they cannot retract their large fleshy siphon into the shell.
Field identification & locations
Identify by its distinctive elongated wing shape with prominent ribs that resemble feathers. Commonly found in coastal areas of the Atlantic and Gulf coasts of North America, particularly in fossil-rich shell beds of Florida.
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