
Slate is a fine-grained metamorphic rock formed from shale under low-grade metamorphism. It splits into thin, flat sheets and has been used for roofing, flooring, and writing surfaces for centuries. Slate's ability to split into thin layers makes it unique among rocks.
| Texture | Foliated (splits into thin sheets) |
| Colors | Gray, black, green, purple, red |
| Magnetism | Non-magnetic |
| Grain Size | Very fine-grained |
| Hardness | 3-4 |
| Density | 2.6-2.9 g/cm³ |
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Main Elements:
Si, Al, K, Fe, O
Chemical Composition:
Similar to shale: clay minerals, quartz, and mica recrystallized under pressure
Slate dust can cause respiratory irritation. Generally safe to handle, but wear masks when cutting.
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Polished: $0.50-$5 per piece
Raw/Tumbled: $1-$10 per piece
Density:
2.6-2.9 g/cm³
Compressive Strength:
100-200 MPa
Melting Point:
Variable
Formation:
Forms when shale is subjected to low-grade metamorphism (heat and pressure), causing the clay minerals to recrystallize and align into parallel layers.
Composition:
Composed of fine-grained mica, quartz, and clay minerals that have been recrystallized under pressure.
Types:
Etymology:
Derived from the Old French word "esclate" meaning "splinter" or "fragment", referring to its tendency to split into thin sheets.
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Uses:
Distribution:
Found worldwide, especially in Wales, Spain, Brazil, and the eastern United States
Historical Use:
Used for roofing and writing surfaces for centuries. School blackboards were originally made of slate!
Symbolism:
Represents education, protection, and transformation
Slate splits into thin sheets because the minerals have been recrystallized and aligned into parallel layers under pressure, creating planes of weakness.
Slate is used for roofing, flooring, writing surfaces (blackboards), billiard tables, and decorative stone due to its ability to split into thin, flat sheets.
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