
Muscovite Mica Specimen
This item is a natural mineral specimen, identified as an aggregate of Muscovite mica, often referred to as 'book mica' due to its distinct layered formation. The specimen exhibits a primary color palette of off-white to creamy translucent hues, characteristic of fresh mica with its pearly to vitreous luster on cleavage planes. Interspersed throughout the intricate structure are areas of lighter brown, tan, and reddish-brown material, which appear to be natural iron staining, oxidized mineral inclusions, or residual matrix from its original geological environment. The overall form is irregularly blocky, stemming from its natural growth habit and subsequent extraction, and is consistent with a hand specimen, roughly estimated to be between 10 to 15 centimeters in its longest dimension. It comprises numerous thin, flexible, and often transparent sheets, showcasing muscovite's perfect basal cleavage. The specimen is presented in its raw, unpolished state, displaying natural rough edges and fractures typical of a mineral found in situ. There are no indications of manufacturing marks, repairs, or significant damage beyond what is inherent to a natural mineral formation and slight surface debris. The clarity and visible definition of individual mica sheets suggest a good quality formation within its natural context, serving as an excellent example of naturally occurring stratified minerals.
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Estimated Value
$75-125
Basic Information
Category
Mineral Specimen
Appraised On
August 28, 2025
Estimated Value
$75-125
Item Description
This item is a natural mineral specimen, identified as an aggregate of Muscovite mica, often referred to as 'book mica' due to its distinct layered formation. The specimen exhibits a primary color palette of off-white to creamy translucent hues, characteristic of fresh mica with its pearly to vitreous luster on cleavage planes. Interspersed throughout the intricate structure are areas of lighter brown, tan, and reddish-brown material, which appear to be natural iron staining, oxidized mineral inclusions, or residual matrix from its original geological environment. The overall form is irregularly blocky, stemming from its natural growth habit and subsequent extraction, and is consistent with a hand specimen, roughly estimated to be between 10 to 15 centimeters in its longest dimension. It comprises numerous thin, flexible, and often transparent sheets, showcasing muscovite's perfect basal cleavage. The specimen is presented in its raw, unpolished state, displaying natural rough edges and fractures typical of a mineral found in situ. There are no indications of manufacturing marks, repairs, or significant damage beyond what is inherent to a natural mineral formation and slight surface debris. The clarity and visible definition of individual mica sheets suggest a good quality formation within its natural context, serving as an excellent example of naturally occurring stratified minerals.
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