
Botryoidal Chalcedony Mineral Specimen
This appears to be a large geode or mineral specimen featuring a prominent formation of botryoidal chalcedony, likely a type of quartz. The overall specimen exhibits a rough, somewhat irregular shape, indicative of a natural formation. The dominant color is a translucent to opaque pale aquamarine or very light blue-green, particularly in the lower and central portions where the chalcedony formations are most concentrated. Towards the top, there is an area of lighter, more opaque white or off-white material, possibly a different mineral or a variation in the chalcedony's purity and structure, possibly indicating a host rock or matrix material. The chalcedony forms grape-like or bubbly aggregates, characteristic of botryoidal habit, with individual spheres or nodules varying in size, creating a textured surface. Some areas show a more drusy, crystalline texture with small, glittering points, especially visible in the lighter regions. There are no discernible manufacturing details, maker's marks, or signatures, strongly suggesting a naturally occurring mineral formation. The condition appears to be good for a natural specimen, with no obvious signs of significant damage like large chips or structural breaks; any irregularities are likely part of its natural growth. The estimated age is geological, as it's a naturally formed mineral. The quality is indicative of a well-formed mineral specimen, showcasing distinct botryoidal habit and a pleasing coloration, making it suitable for display in a mineral collection.
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Estimated Value
$150-250
Basic Information
Category
Mineral Specimen
Appraised On
August 28, 2025
Estimated Value
$150-250
Additional Details Provided By Owner
User Provided Information
4 x 3
Item Description
This appears to be a large geode or mineral specimen featuring a prominent formation of botryoidal chalcedony, likely a type of quartz. The overall specimen exhibits a rough, somewhat irregular shape, indicative of a natural formation. The dominant color is a translucent to opaque pale aquamarine or very light blue-green, particularly in the lower and central portions where the chalcedony formations are most concentrated. Towards the top, there is an area of lighter, more opaque white or off-white material, possibly a different mineral or a variation in the chalcedony's purity and structure, possibly indicating a host rock or matrix material. The chalcedony forms grape-like or bubbly aggregates, characteristic of botryoidal habit, with individual spheres or nodules varying in size, creating a textured surface. Some areas show a more drusy, crystalline texture with small, glittering points, especially visible in the lighter regions. There are no discernible manufacturing details, maker's marks, or signatures, strongly suggesting a naturally occurring mineral formation. The condition appears to be good for a natural specimen, with no obvious signs of significant damage like large chips or structural breaks; any irregularities are likely part of its natural growth. The estimated age is geological, as it's a naturally formed mineral. The quality is indicative of a well-formed mineral specimen, showcasing distinct botryoidal habit and a pleasing coloration, making it suitable for display in a mineral collection.
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