
Shale is a fine-grained sedimentary rock formed from compressed mud and clay. It splits into thin layers and is the most common sedimentary rock. Shale is important as a source rock for oil and natural gas, making it economically significant worldwide.
| Texture | Laminated (splits into layers) |
| Colors | Gray, black, brown, red, green |
| Magnetism | Non-magnetic |
| Grain Size | Very fine-grained |
| Hardness | 2-4 |
| Density | 2.0-2.7 g/cm³ |
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Main Elements:
Si, Al, O, K, Fe
Chemical Composition:
Variable, primarily clay minerals (kaolinite, illite) and quartz, with organic matter
Shale dust can cause respiratory irritation. Generally safe to handle, but avoid inhaling fine particles.
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Polished: $0.10-$1 per piece
Raw/Tumbled: $0.50-$3 per piece
Density:
2.0-2.7 g/cm³
Compressive Strength:
10-100 MPa
Melting Point:
Variable
Formation:
Forms from compressed mud and clay in quiet water environments like lakes, lagoons, and deep ocean basins.
Composition:
Composed mainly of clay minerals, quartz, and organic matter. The most common sedimentary rock.
Types:
Etymology:
Derived from the Old English word "scealu" meaning "shell" or "husk", referring to its tendency to split into thin layers.
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Uses:
Distribution:
Found worldwide, the most common sedimentary rock on Earth
Historical Use:
Used for thousands of years in pottery and brick making. Modern fracking extracts oil and gas from shale formations.
Symbolism:
Represents layers of time and Earth's history
Shale is the most common sedimentary rock and is a major source rock for oil and natural gas. It's also used in construction and pottery.
Shale is a sedimentary rock that splits into layers. When shale is subjected to heat and pressure, it becomes slate, a metamorphic rock.
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