
Phlogopite Mica Specimen
This item is a raw, natural crystalline mineral specimen, specifically a variety of mica known as Phlogopite. It measures approximately 2 to 3 centimeters in length, held between fingertips for scale. Physically, it exhibits a distinctively vitreous to pearly luster with a rich, metallic golden-bronze to yellowish-brown coloration. The construction of the specimen is characterized by its book-like, foliated crystal structure, consisting of numerous thin, flexible, and elastic laminae or sheets stacked together. This creates a highly reflective, prismatic surface that catches the light from various angles. The edges appear somewhat jagged and irregular, typical of a piece that has been extracted from a larger rock matrix. There are darker inclusions of matrix material at the base, likely iron or magnesium-rich silicates. In terms of condition, the specimen shows some fraying and minor delamination along the edges of the plates, which is a common natural occurrence for mica due to its perfect basal cleavage. There are no signs of synthetic treatment or man-made coatings; it appears to be in its natural geological state. As a geological specimen, it lacks maker's marks, but its formation suggests origins from a magnesium-rich metamorphic environment such as marble or pegmatite. The high degree of translucency in thinner flakes and the intense golden sheen indicate a high-quality mineralogical sample.
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Estimated Value
$15.00 - $25.00
Basic Information
Category
Minerals and Geological Specimens
Appraised On
April 15, 2026
Estimated Value
$15.00 - $25.00
Item Description
This item is a raw, natural crystalline mineral specimen, specifically a variety of mica known as Phlogopite. It measures approximately 2 to 3 centimeters in length, held between fingertips for scale. Physically, it exhibits a distinctively vitreous to pearly luster with a rich, metallic golden-bronze to yellowish-brown coloration. The construction of the specimen is characterized by its book-like, foliated crystal structure, consisting of numerous thin, flexible, and elastic laminae or sheets stacked together. This creates a highly reflective, prismatic surface that catches the light from various angles. The edges appear somewhat jagged and irregular, typical of a piece that has been extracted from a larger rock matrix. There are darker inclusions of matrix material at the base, likely iron or magnesium-rich silicates. In terms of condition, the specimen shows some fraying and minor delamination along the edges of the plates, which is a common natural occurrence for mica due to its perfect basal cleavage. There are no signs of synthetic treatment or man-made coatings; it appears to be in its natural geological state. As a geological specimen, it lacks maker's marks, but its formation suggests origins from a magnesium-rich metamorphic environment such as marble or pegmatite. The high degree of translucency in thinner flakes and the intense golden sheen indicate a high-quality mineralogical sample.
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