Polished Banded Agate Nodule
Rocks, Fossils & Minerals

Polished Banded Agate Nodule

This specimen is a natural banded agate nodule, likely a variety of Lake Superior or carnelian-style agate, held in a person's hand for scale (approximately 2 to 2.5 inches in length). The stone displays classic microcrystalline quartz characteristics with distinct concentric banding. The color palette is rich and warm, featuring translucent layers of honey-amber, deep butterscotch, and creamy white, with a subtle hint of grayish-blue chalcedony near the top. The surface appears to have a semi-polished or naturally smooth waxy texture, suggesting it may have been tumbled or water-worn. The physical construction is a solid, dense mineral mass with a slightly irregular, rounded shape. Notable features include the high contrast between the opaque yellow-orange bands and the more translucent internal layers. Regarding condition, the stone shows some natural surface pitting, micro-fractures, and minor chips along the edges, which are common for raw or lightly processed gemstones. There are no visible maker's marks, as it is a natural geological formation. The quality is indicative of a high-grade collector's specimen due to the clarity of the banding and the saturation of the iron-oxide-derived coloring. Its age dates back millions of years to the volcanic activities that formed the air bubbles in which these crystals grew.

Estimated Value

$25.00 - $45.00

Basic Information

Category

Rocks, Fossils & Minerals

Appraised On

March 18, 2026

Estimated Value

$25.00 - $45.00

Item Description

This specimen is a natural banded agate nodule, likely a variety of Lake Superior or carnelian-style agate, held in a person's hand for scale (approximately 2 to 2.5 inches in length). The stone displays classic microcrystalline quartz characteristics with distinct concentric banding. The color palette is rich and warm, featuring translucent layers of honey-amber, deep butterscotch, and creamy white, with a subtle hint of grayish-blue chalcedony near the top. The surface appears to have a semi-polished or naturally smooth waxy texture, suggesting it may have been tumbled or water-worn. The physical construction is a solid, dense mineral mass with a slightly irregular, rounded shape. Notable features include the high contrast between the opaque yellow-orange bands and the more translucent internal layers. Regarding condition, the stone shows some natural surface pitting, micro-fractures, and minor chips along the edges, which are common for raw or lightly processed gemstones. There are no visible maker's marks, as it is a natural geological formation. The quality is indicative of a high-grade collector's specimen due to the clarity of the banding and the saturation of the iron-oxide-derived coloring. Its age dates back millions of years to the volcanic activities that formed the air bubbles in which these crystals grew.

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