
Amphibolite is a metamorphic rock composed mainly of amphibole minerals (especially hornblende) and plagioclase feldspar. It forms from basalt or other mafic rocks under medium to high-grade metamorphism. Amphibolite is dark-colored and often displays a foliated texture.
| Texture | Foliated to massive |
| Colors | Dark green, black, dark gray |
| Magnetism | Non-magnetic |
| Grain Size | Medium to coarse-grained |
| Hardness | 6-7 |
| Density | 2.9-3.2 g/cm³ |
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Main Elements:
Si, Al, Ca, Fe, Mg, O
Chemical Composition:
Similar to basalt: hornblende (amphibole), plagioclase feldspar, with minor quartz and biotite
Amphibolite dust can cause respiratory irritation. Contains silica, so wear protective masks when cutting.
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Polished: $0.50-$4 per piece
Raw/Tumbled: $2-$10 per piece
Density:
2.9-3.2 g/cm³
Compressive Strength:
100-300 MPa
Melting Point:
Variable
Formation:
Forms when basalt or other mafic rocks are subjected to medium to high-grade metamorphism, causing the minerals to recrystallize into amphibole and plagioclase.
Composition:
Composed mainly of hornblende (amphibole mineral) and plagioclase feldspar, with minor amounts of quartz and biotite.
Types:
Etymology:
Named for its dominant mineral, amphibole, which comes from the Greek "amphibolos" meaning "ambiguous" or "doubtful".
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Uses:
Distribution:
Found worldwide in metamorphic terrains, especially in mountain ranges
Historical Use:
Used in construction and as decorative stone. Important for understanding Earth's tectonic processes.
Symbolism:
Represents transformation and Earth's deep processes
Amphibolite is used in construction, decorative stone, and railway ballast due to its durability and attractive dark appearance.
Amphibolite forms when basalt or other mafic rocks are subjected to medium to high-grade metamorphism, recrystallizing into amphibole and plagioclase minerals.
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