Rough Pale Green Gemstone Specimen
Minerals and Gemstones

Rough Pale Green Gemstone Specimen

This specimen is a raw, unpolished mineral fragment of a pale, yellowish-green hue, measuring approximately 1.5 to 2 centimeters in length. The material exhibits a translucent to semi-opaque quality with a waxy to vitreous luster, characteristic of minerals like green calcite, prehnite, or low-grade jadeite. The physical structure shows a conchoidal to irregular fracture pattern, typical of non-crystalline or microcrystalline structures. The color is distributed relatively evenly but appears lighter in thinner, more translucent sections. Notable features include a network of fine surfacing abrasions and white scuff marks across the primary faces, likely caused by contact with harder materials or rough handling. There are no discerning maker's marks or signatures, as this is a natural geological specimen rather than a manufactured object. The condition is raw and 'as-found,' with sharp, jagged edges that have not been tumbled or faceted. The quality of the material is consistent with lapidary rough or a amateur mineral collector's sample. Its age is geological, though its extraction is likely contemporary based on the freshness of the fractured surfaces.

Estimated Value

$5.00 - $12.00

Basic Information

Category

Minerals and Gemstones

Appraised On

March 12, 2026

Estimated Value

$5.00 - $12.00

Item Description

This specimen is a raw, unpolished mineral fragment of a pale, yellowish-green hue, measuring approximately 1.5 to 2 centimeters in length. The material exhibits a translucent to semi-opaque quality with a waxy to vitreous luster, characteristic of minerals like green calcite, prehnite, or low-grade jadeite. The physical structure shows a conchoidal to irregular fracture pattern, typical of non-crystalline or microcrystalline structures. The color is distributed relatively evenly but appears lighter in thinner, more translucent sections. Notable features include a network of fine surfacing abrasions and white scuff marks across the primary faces, likely caused by contact with harder materials or rough handling. There are no discerning maker's marks or signatures, as this is a natural geological specimen rather than a manufactured object. The condition is raw and 'as-found,' with sharp, jagged edges that have not been tumbled or faceted. The quality of the material is consistent with lapidary rough or a amateur mineral collector's sample. Its age is geological, though its extraction is likely contemporary based on the freshness of the fractured surfaces.

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