
Basalt is a dark-colored, fine-grained igneous rock that forms from rapidly cooled lava. It is one of the most common rocks on Earth, forming the ocean floor and many volcanic islands. Basalt's dark appearance comes from its high iron and magnesium content, making it denser than granite.
| Texture | Aphanitic |
| Colors | Dark gray to black |
| Magnetism | Magnetic (due to iron content) |
| Grain Size | Fine-grained |
| Hardness | 6 – 7 |
| Density | 2.8 – 3.0 g/cm³ |
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Main Elements:
Si, Al, Fe, Mg, Ca, Na, K, O
Chemical Composition:
SiO₂ 45-52%, Al₂O₃ 14-18%, FeO 5-14%, MgO 5-12%, CaO 8-12%, Na₂O 2-5%, K₂O 0.5-2%, TiO₂ 1-3%
Basalt dust from cutting or grinding can cause respiratory irritation. The fine particles may contain crystalline silica. Wear protective masks when working with basalt.
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Polished: $0.10 – $0.50 per piece
Raw/Tumbled: $1 – $5 per piece
Density:
2.8 – 3.0 g/cm³
Compressive Strength:
100 – 300 MPa
Melting Point:
1000 – 1200°C
Formation:
Forms from rapidly cooled lava flows, either on the surface (extrusive) or in shallow intrusions. Most common rock type on ocean floors.
Composition:
Composed mainly of plagioclase feldspar and pyroxene minerals, with olivine and magnetite.
Types:
Etymology:
Derived from the Latin word "basaltes", possibly from an ancient Ethiopian word meaning "black stone".
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Uses:
Distribution:
Found worldwide, especially in volcanic regions and ocean floors
Historical Use:
Used by ancient peoples for tools and weapons. The Giant's Causeway in Ireland is a famous basalt formation.
Symbolism:
Represents volcanic power and Earth's dynamic nature
Basalt is commonly used in road construction, as concrete aggregate, railway ballast, and in building materials due to its durability.
Basalt is found worldwide, especially in volcanic regions like Iceland, Hawaii, and India. It forms most of the ocean floor.
Yes, basalt can be magnetic due to its iron content, particularly magnetite minerals within the rock.
Basalt forms when lava cools rapidly, either on the Earth's surface or in shallow intrusions, preventing large crystals from forming.
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