Phlogopite or Muscovite Mica Specimen
Rocks, Fossils & Minerals / Geological Specimens

Phlogopite or Muscovite Mica Specimen

This is a raw mineral specimen, specifically a variety of mica, likely phlogopite or muscovite. The object is a small, hand-held specimen approximately 2-3 centimeters in length with an irregular, elongated oval shape. It exhibits the classic 'book-like' foliated structure characteristic of phyllosilicate minerals, where thin, flexible sheets are stacked atop one another. The color ranges from a Pale metallic gold and brassy yellow to deeper bronze and olive-brown tones, giving it a prominent pearly to sub-metallic luster under direct light. The piece shows significant surface texture with jagged, uneven edges where individual lamellae have been bent or fractured. There is visible darker matrix material or oxidation embedded within the crevices of the sheets. Its condition is consistent with a raw field-collected mineral, showing edge wear and slight delamination of the layers. As a natural geological specimen, there are no maker's marks or signatures. Its age is geological, potentially hundreds of millions of years old. The quality is a standard study-grade mineral sample, notable for its reflective properties and distinct monoclinic crystal habit exhibited in its layering.

Estimated Value

$10.00 - $25.00

Basic Information

Category

Rocks, Fossils & Minerals / Geological Specimens

Appraised On

April 15, 2026

Estimated Value

$10.00 - $25.00

Item Description

This is a raw mineral specimen, specifically a variety of mica, likely phlogopite or muscovite. The object is a small, hand-held specimen approximately 2-3 centimeters in length with an irregular, elongated oval shape. It exhibits the classic 'book-like' foliated structure characteristic of phyllosilicate minerals, where thin, flexible sheets are stacked atop one another. The color ranges from a Pale metallic gold and brassy yellow to deeper bronze and olive-brown tones, giving it a prominent pearly to sub-metallic luster under direct light. The piece shows significant surface texture with jagged, uneven edges where individual lamellae have been bent or fractured. There is visible darker matrix material or oxidation embedded within the crevices of the sheets. Its condition is consistent with a raw field-collected mineral, showing edge wear and slight delamination of the layers. As a natural geological specimen, there are no maker's marks or signatures. Its age is geological, potentially hundreds of millions of years old. The quality is a standard study-grade mineral sample, notable for its reflective properties and distinct monoclinic crystal habit exhibited in its layering.

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