Many fossils of shelly organisms (e.g., bivalves, gastropods, brachiopods, cephalopods) have had the original hard parts dissolved away. In such cases, the fossil itself is an impression of the outside of the shell (external mold) or an impression of the inside of the shell (internal mold).
Hormotoma (Mollusca, Gastropoda, Archaeogastropoda, Murchisonioidea, Murchisoniidae) (4.9 cm tall) - this fossil snail from eastern Iowa is preserved as an internal mold (= the coiled portion; fine-grained sediment has filled up the originally-hollow shell) and as an external mold (= the cavity in which the coil sits). Note the gap between the external & internal molds - that's where the original CaCO3 shell was.
Matrix: weathered fossiliferous limestone
Stratigraphy: Galena Formation, upper Middle Ordovician to lower Upper Ordovician
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{{Information |Description=Many fossils of shelly organisms (e.g., bivalves, gastropods, brachiopods, cephalopods) have had the original hard parts dissolved away. In such cases, the fossil itself is an impression of the outside of the shell (external...
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