Botryoidal Chalcedony and Quartz Specimen
Mineral Specimen

Botryoidal Chalcedony and Quartz Specimen

The item is a small, irregularly shaped geode or mineral specimen, currently being held in the palm of a hand for scale. Its primary composition appears to be a type of chalcedony or agate, exhibiting a milky white to translucent coloration. The surface is highly textured, featuring botryoidal formations, which are rounded, grape-like clusters. There are also areas with crystalline structures, likely quartz points, visible on the upper and lower edges. The specimen shows some natural inclusions and surface imperfections, possibly iron staining or other mineral deposits, giving it a slightly brownish or grayish hue in certain areas. There is visible dirt and debris adhering to the surface, suggesting it is a raw or uncleaned specimen. No man-made alterations, repairs, or identifying marks such as manufacturing stamps or signatures are apparent. The overall form suggests a natural geological formation, possibly found in a geode nodule or as part of a larger vein deposit. The quality of the crystallization and botryoidal formation appears typical for this type of mineral. The age is geological, likely millions of years old.

Estimated Value

$20-40

Basic Information

Category

Mineral Specimen

Appraised On

August 28, 2025

Estimated Value

$20-40

Item Description

The item is a small, irregularly shaped geode or mineral specimen, currently being held in the palm of a hand for scale. Its primary composition appears to be a type of chalcedony or agate, exhibiting a milky white to translucent coloration. The surface is highly textured, featuring botryoidal formations, which are rounded, grape-like clusters. There are also areas with crystalline structures, likely quartz points, visible on the upper and lower edges. The specimen shows some natural inclusions and surface imperfections, possibly iron staining or other mineral deposits, giving it a slightly brownish or grayish hue in certain areas. There is visible dirt and debris adhering to the surface, suggesting it is a raw or uncleaned specimen. No man-made alterations, repairs, or identifying marks such as manufacturing stamps or signatures are apparent. The overall form suggests a natural geological formation, possibly found in a geode nodule or as part of a larger vein deposit. The quality of the crystallization and botryoidal formation appears typical for this type of mineral. The age is geological, likely millions of years old.

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