
Chert (Flint) Specimen with Inclusion
The item is a specimen of chert, also known as flint. It is an irregularly shaped piece, approximately 3-4 inches in its longest dimension, held between two fingers in the image, giving a sense of its size relative to a hand. The material appears to be cryptocrystalline quartz, exhibiting a conchoidal fracture pattern on several surfaces, characteristic of chert. The color is predominantly a pale, off-white or creamy white with some areas appearing translucent. A notable feature is the presence of a distinct band or inclusion running vertically down the left side of the specimen. This inclusion is a darker, reddish-brown color and has a porous or granular texture, contrasting sharply with the surrounding chert. This could represent a layer of host rock or a weathered inclusion. There are numerous small fractures or fissures visible across the surface, suggesting some degree of weathering or perhaps impact damage. The overall condition appears stable, with no immediate signs of crumbling, although the porous inclusion may be more fragile. There are no visible maker's marks or signatures, as expected for a natural geological specimen. The specimen’s characteristics point to its natural formation over geologic time, likely dating back millions of years depending on the specific geological context from which it was collected. The interplay of the pale chert and the darker inclusion creates a visually interesting contrast, adding to its appeal as a geological sample. The quality of the chert itself, while fractured on the surface, shows the potential for sharp edges upon breakage, typical of high-quality flint used historically for tools.
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Estimated Value
$15-25
Basic Information
Category
Mineral Specimen
Appraised On
August 28, 2025
Estimated Value
$15-25
Item Description
The item is a specimen of chert, also known as flint. It is an irregularly shaped piece, approximately 3-4 inches in its longest dimension, held between two fingers in the image, giving a sense of its size relative to a hand. The material appears to be cryptocrystalline quartz, exhibiting a conchoidal fracture pattern on several surfaces, characteristic of chert. The color is predominantly a pale, off-white or creamy white with some areas appearing translucent. A notable feature is the presence of a distinct band or inclusion running vertically down the left side of the specimen. This inclusion is a darker, reddish-brown color and has a porous or granular texture, contrasting sharply with the surrounding chert. This could represent a layer of host rock or a weathered inclusion. There are numerous small fractures or fissures visible across the surface, suggesting some degree of weathering or perhaps impact damage. The overall condition appears stable, with no immediate signs of crumbling, although the porous inclusion may be more fragile. There are no visible maker's marks or signatures, as expected for a natural geological specimen. The specimen’s characteristics point to its natural formation over geologic time, likely dating back millions of years depending on the specific geological context from which it was collected. The interplay of the pale chert and the darker inclusion creates a visually interesting contrast, adding to its appeal as a geological sample. The quality of the chert itself, while fractured on the surface, shows the potential for sharp edges upon breakage, typical of high-quality flint used historically for tools.
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