
Scoria is a dark-colored, vesicular volcanic rock that forms from mafic lava. Unlike pumice, scoria is denser and sinks in water. It has a rough, cinder-like appearance and is commonly used in landscaping and as lightweight aggregate.
| Texture | Vesicular (bubbly) |
| Colors | Dark brown, black, dark red |
| Magnetism | Potentially magnetic |
| Grain Size | Fine to medium-grained |
| Hardness | 5-6 |
| Density | 1.5-2.5 g/cm³ |
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Main Elements:
Si, Al, Fe, Mg, Ca, O
Chemical Composition:
SiO₂ 45-52%, Al₂O₃ 14-18%, FeO 5-14%, MgO 5-12%, CaO 8-12%, similar to basalt
Scoria dust can cause respiratory irritation. Generally safe to handle, but avoid inhaling fine particles.
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Polished: $0.10-$0.80 per piece
Raw/Tumbled: $0.50-$4 per piece
Density:
1.5-2.5 g/cm³
Compressive Strength:
Low (highly porous)
Melting Point:
1000-1200°C
Formation:
Forms when gas-rich mafic lava erupts, trapping gas bubbles as the lava cools. The darker color comes from iron-rich minerals.
Composition:
Composed of volcanic glass with gas bubbles, similar in composition to basalt but with trapped gas.
Types:
Etymology:
Derived from the Greek word "skoria" meaning "dross" or "refuse", referring to its cinder-like appearance.
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Uses:
Distribution:
Found in volcanic regions worldwide, especially around cinder cone volcanoes
Historical Use:
Used in construction and landscaping. Cinder cones are made entirely of scoria.
Symbolism:
Represents volcanic activity and Earth's fiery nature
Scoria is darker, denser, and sinks in water, while pumice is lighter, lighter in color, and floats. Scoria forms from mafic lava, pumice from felsic lava.
Scoria is found around cinder cone volcanoes and volcanic regions worldwide, especially in areas with basaltic volcanism.
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