Foliated Metamorphic Rock Fragment (Schist/Phyllite)
Mineral Specimen

Foliated Metamorphic Rock Fragment (Schist/Phyllite)

The item is an irregular, elongated piece of a dark grey to black mineral, likely a schist or similar metamorphic rock, characterized by its distinctly foliated or schistose texture. It measures approximately 3-4 inches in length and appears to fit comfortably within the palm of a hand. The primary color is a dark, muted grey, almost black, with lighter grey to silvery streaks and patches, indicative of mineral cleavage planes or inclusions. The surface is uneven and fractured, showing natural breaks rather than deliberate cuts, with some areas exhibiting a subtle, almost metallic luster where surfaces have fractured along mineral planes. Small flecks of what appear to be mica or a similar platy mineral are visible throughout, contributing to the shimmering quality in certain light conditions. There are no discernible manufacturing details, maker's marks, or artificial modifications, suggesting it is a natural specimen. The condition appears to be stable, with typical wear and fracturing expected of a natural rock or mineral fragment, but no signs of recent damage, repairs, or significant weathering. Given its unrefined state, it doesn't adhere to a specific style period but represents a natural geological formation. The quality is indicative of a common natural mineral specimen, valuable for geological study or collection due to its clear exhibition of schistosity.

Estimated Value

$5-15

Basic Information

Category

Mineral Specimen

Appraised On

August 30, 2025

Estimated Value

$5-15

Item Description

The item is an irregular, elongated piece of a dark grey to black mineral, likely a schist or similar metamorphic rock, characterized by its distinctly foliated or schistose texture. It measures approximately 3-4 inches in length and appears to fit comfortably within the palm of a hand. The primary color is a dark, muted grey, almost black, with lighter grey to silvery streaks and patches, indicative of mineral cleavage planes or inclusions. The surface is uneven and fractured, showing natural breaks rather than deliberate cuts, with some areas exhibiting a subtle, almost metallic luster where surfaces have fractured along mineral planes. Small flecks of what appear to be mica or a similar platy mineral are visible throughout, contributing to the shimmering quality in certain light conditions. There are no discernible manufacturing details, maker's marks, or artificial modifications, suggesting it is a natural specimen. The condition appears to be stable, with typical wear and fracturing expected of a natural rock or mineral fragment, but no signs of recent damage, repairs, or significant weathering. Given its unrefined state, it doesn't adhere to a specific style period but represents a natural geological formation. The quality is indicative of a common natural mineral specimen, valuable for geological study or collection due to its clear exhibition of schistosity.

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