Quartz Crystal Cluster
Mineral Specimen

Quartz Crystal Cluster

This appears to be a large cluster of quartz crystals, likely a substantial geode or a portion of a larger crystalline formation. The cluster exhibits numerous individual crystals of varying sizes, predominantly in the range of a few millimeters to perhaps 2 centimeters across at their visible faces. The crystals are generally clear or translucent, displaying the characteristic hexagonal prismatic form with pyramidal terminations of quartz. There are numerous inclusions or stains visible within the cluster, rendering some areas a pale orange or reddish-brown hue, which may be caused by iron oxides or other minerals. The base material, upon which the crystals are formed, appears to be a host rock or massive crystalline formation. The overall shape is irregular and volumetric, suggesting it was removed from its natural setting. There are no obvious signs of significant damage such as large fractures or chips, though some abrasion to the smaller crystal points is likely given its natural state. The quality of the individual crystals appears reasonably good with notable transparency, although the density of smaller crystals may limit the view of larger, more perfectly formed specimens within the cluster. There are no visible maker's marks, signatures, or stamps, consistent with a natural mineral specimen. The size is substantial, occupying a significant portion of the surface it rests upon. The craftsmanship is entirely natural.

Estimated Value

$300-500

Basic Information

Category

Mineral Specimen

Appraised On

August 28, 2025

Estimated Value

$300-500

Item Description

This appears to be a large cluster of quartz crystals, likely a substantial geode or a portion of a larger crystalline formation. The cluster exhibits numerous individual crystals of varying sizes, predominantly in the range of a few millimeters to perhaps 2 centimeters across at their visible faces. The crystals are generally clear or translucent, displaying the characteristic hexagonal prismatic form with pyramidal terminations of quartz. There are numerous inclusions or stains visible within the cluster, rendering some areas a pale orange or reddish-brown hue, which may be caused by iron oxides or other minerals. The base material, upon which the crystals are formed, appears to be a host rock or massive crystalline formation. The overall shape is irregular and volumetric, suggesting it was removed from its natural setting. There are no obvious signs of significant damage such as large fractures or chips, though some abrasion to the smaller crystal points is likely given its natural state. The quality of the individual crystals appears reasonably good with notable transparency, although the density of smaller crystals may limit the view of larger, more perfectly formed specimens within the cluster. There are no visible maker's marks, signatures, or stamps, consistent with a natural mineral specimen. The size is substantial, occupying a significant portion of the surface it rests upon. The craftsmanship is entirely natural.

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