
Phyllite is a metamorphic rock intermediate between slate and schist. It has a silky sheen due to fine-grained mica and displays a foliated texture. Phyllite forms from shale under medium-grade metamorphism and is often used as decorative stone.
| Texture | Foliated (silky sheen) |
| Colors | Gray, green, black (with silky luster) |
| Magnetism | Non-magnetic |
| Grain Size | Fine-grained |
| Hardness | 2-4 |
| Density | 2.6-2.9 g/cm³ |
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Main Elements:
Si, Al, K, Fe, Mg, O
Chemical Composition:
Similar to slate: fine-grained mica, quartz, and clay minerals, more recrystallized than slate
Phyllite dust can cause respiratory irritation. Generally safe to handle, but wear masks when cutting.
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Polished: $0.40-$3 per piece
Raw/Tumbled: $1-$8 per piece
Density:
2.6-2.9 g/cm³
Compressive Strength:
Variable
Melting Point:
Variable
Formation:
Forms when shale is subjected to medium-grade metamorphism, more intense than slate but less than schist. The mica begins to recrystallize, creating a silky sheen.
Composition:
Composed of fine-grained mica, quartz, and clay minerals that have been partially recrystallized, giving it a silky appearance.
Types:
Etymology:
Derived from the Greek word "phyllon" meaning "leaf", referring to its foliated, leaf-like texture.
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Uses:
Distribution:
Found worldwide in medium-grade metamorphic terrains
Historical Use:
Used as decorative stone and roofing material. Less common than slate or schist.
Symbolism:
Represents transition, transformation, and intermediate stages
Slate is the lowest grade (fine-grained, no sheen), phyllite is intermediate (silky sheen), and schist is highest grade (coarse-grained, very shiny).
Phyllite's silky sheen comes from fine-grained mica minerals that have begun to recrystallize, reflecting light in a characteristic way.
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