Calcite Crystal with Sphalerite Matrix
Geological Specimens and Minerals

Calcite Crystal with Sphalerite Matrix

This specimen is a large, translucent to semi-opaque mineral cluster, specifically identified as honey calcite (calcite). The crystal exhibits a distinct scale-like or rhombohedral cleavage structure characteristic of the carbonate mineral class. Its primary coloration ranges from a light pale cream to a deep honey-yellow and amber hue, likely caused by iron inclusions or similar trace elements. The specimen measures approximately several inches across and possesses a waxy to vitreous luster. Attached to the lower right side is a dark, metallic-gray matrix, which appears to be mineralized rock, potentially containing galena or sphalerite, common associates for this type of geode-based crystal growth. The edges of the calcite show some rough fracturing and contact points where it was harvested from its original rock pocket. The physical condition reflects natural geological formation, with no signs of synthetic enhancement or machine polishing. The sharpness of the crystal terminations and the contrast between the luminous calcite and the dark, textured host rock suggest a high-quality decorative or collector-grade mineral specimen. No maker's marks or signatures are present, as this is a natural geological occurrence. The specimen likely originates from a known mining district, possibly in the American Midwest or Mexico, where honey calcite is frequently found in hydrothermal vein deposits.

Estimated Value

$150 - $250

Basic Information

Category

Geological Specimens and Minerals

Appraised On

May 2, 2026

Estimated Value

$150 - $250

Item Description

This specimen is a large, translucent to semi-opaque mineral cluster, specifically identified as honey calcite (calcite). The crystal exhibits a distinct scale-like or rhombohedral cleavage structure characteristic of the carbonate mineral class. Its primary coloration ranges from a light pale cream to a deep honey-yellow and amber hue, likely caused by iron inclusions or similar trace elements. The specimen measures approximately several inches across and possesses a waxy to vitreous luster. Attached to the lower right side is a dark, metallic-gray matrix, which appears to be mineralized rock, potentially containing galena or sphalerite, common associates for this type of geode-based crystal growth. The edges of the calcite show some rough fracturing and contact points where it was harvested from its original rock pocket. The physical condition reflects natural geological formation, with no signs of synthetic enhancement or machine polishing. The sharpness of the crystal terminations and the contrast between the luminous calcite and the dark, textured host rock suggest a high-quality decorative or collector-grade mineral specimen. No maker's marks or signatures are present, as this is a natural geological occurrence. The specimen likely originates from a known mining district, possibly in the American Midwest or Mexico, where honey calcite is frequently found in hydrothermal vein deposits.

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