Mica Schist Geological Specimen
Geological Specimens / Rocks & Minerals

Mica Schist Geological Specimen

This item is a medium-grained metamorphic rock specimen, specifically identified as mica schist. The piece measures approximately 4-5 inches in length with a flattened, tabular geometry characteristic of regional metamorphism. The primary physical characteristic is its strong foliation, or 'schistosity,' which is visible as distinct layering and parallel alignment of mineral grains. The color palette across the surface is a complex mix of silvery-gray, dull green, and significant yellowish-ochre iron oxide staining, indicating prolonged exposure to moisture and weathering. The silvery sheen is caused by a high concentration of muscovite or biotite mica flakes, which align to create a glittering effect when the piece is rotated in the light. The construction is entirely natural, formed deep within the Earth's crust under intense heat and pressure, likely dating back millions of years. Notable features include the uneven, jagged edges on the left side where the rock has cleaved along its natural planes of weakness. There are no man-made markings, signatures, or stamps, as this is a raw natural specimen. The condition is raw and weathered; the surface is rough to the touch with visible pitting and sedimentary-like deposits of oxidation. Its craftsmanship is provided by nature, showcasing the high-quality crystallization of silicate minerals characteristic of high-grade metamorphic environments.

Estimated Value

$15.00 - $25.00

Basic Information

Category

Geological Specimens / Rocks & Minerals

Appraised On

April 12, 2026

Estimated Value

$15.00 - $25.00

Item Description

This item is a medium-grained metamorphic rock specimen, specifically identified as mica schist. The piece measures approximately 4-5 inches in length with a flattened, tabular geometry characteristic of regional metamorphism. The primary physical characteristic is its strong foliation, or 'schistosity,' which is visible as distinct layering and parallel alignment of mineral grains. The color palette across the surface is a complex mix of silvery-gray, dull green, and significant yellowish-ochre iron oxide staining, indicating prolonged exposure to moisture and weathering. The silvery sheen is caused by a high concentration of muscovite or biotite mica flakes, which align to create a glittering effect when the piece is rotated in the light. The construction is entirely natural, formed deep within the Earth's crust under intense heat and pressure, likely dating back millions of years. Notable features include the uneven, jagged edges on the left side where the rock has cleaved along its natural planes of weakness. There are no man-made markings, signatures, or stamps, as this is a raw natural specimen. The condition is raw and weathered; the surface is rough to the touch with visible pitting and sedimentary-like deposits of oxidation. Its craftsmanship is provided by nature, showcasing the high-quality crystallization of silicate minerals characteristic of high-grade metamorphic environments.

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