
How can you tell if a fossil is real?
A real fossil usually shows repeated biological structure, consistent mineral replacement or preservation, and a believable relationship to the surrounding matrix. It should not look randomly decorative in only one spot. Real shells keep patterned ribbing and symmetry, real bone often shows internal pore structure, and petrified wood preserves grain or growth-ring logic. The reliable standard is not one magic test but a combination of structure, hardness, context, and whether the specimen makes geologic sense for the site where it was found.
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