
Geode or Vug Specimen
The item is a mineral specimen, likely a geode or vug, presenting as a roughly oval-shaped piece of rock. It measures approximately 8-10 inches in length and exhibits a dark reddish-brown, porous exterior matrix, consistent with volcanic rock or basalts. Several areas on the surface reveal internal crystalline formations, appearing pale blue or white and exhibiting a botryoidal or mammillary habit, which are characteristic of chalcedony or agate. There are visible small voids and cavities on the exterior. Some areas of the exterior show a reddish-orange staining, likely due to iron content. White, powdery residues or mineral deposits are present in several locations, particularly around the exposed crystal formations. Small pieces of organic material or debris are also visible on the surface, embedded in the pores. No apparent manufacturing marks, signatures, or stamps are discernible. The condition appears to be natural, consistent with a specimen collected from the earth, showing natural wear and possible cleavage along crystalline planes. The age is geologically determined, not a manufactured item. The quality lies in the interesting contrast between the rough exterior matrix and the potentially crystalline interior. It is a raw, unpolished specimen.
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Estimated Value
$30 - $60
Basic Information
Category
Minerals and Rocks
Appraised On
August 28, 2025
Estimated Value
$30 - $60
Item Description
The item is a mineral specimen, likely a geode or vug, presenting as a roughly oval-shaped piece of rock. It measures approximately 8-10 inches in length and exhibits a dark reddish-brown, porous exterior matrix, consistent with volcanic rock or basalts. Several areas on the surface reveal internal crystalline formations, appearing pale blue or white and exhibiting a botryoidal or mammillary habit, which are characteristic of chalcedony or agate. There are visible small voids and cavities on the exterior. Some areas of the exterior show a reddish-orange staining, likely due to iron content. White, powdery residues or mineral deposits are present in several locations, particularly around the exposed crystal formations. Small pieces of organic material or debris are also visible on the surface, embedded in the pores. No apparent manufacturing marks, signatures, or stamps are discernible. The condition appears to be natural, consistent with a specimen collected from the earth, showing natural wear and possible cleavage along crystalline planes. The age is geologically determined, not a manufactured item. The quality lies in the interesting contrast between the rough exterior matrix and the potentially crystalline interior. It is a raw, unpolished specimen.
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