
igneous
Basalt (River Stone)
Aphanitic Mafic Igneous Rock
Hardness: 6 (Mohs scale); Color: Dark grey to charcoal black; Luster: Dull to sub-metallic; Crystal structure: Microcrystalline (aphanitic); Cleavage: None; Specific gravity: 2.8–3.0
- Hardness
- 6 (Mohs scale)
- Color
- Dark grey to charcoal black
- Luster
- Dull to sub-metallic
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Physical properties
Hardness: 6 (Mohs scale); Color: Dark grey to charcoal black; Luster: Dull to sub-metallic; Crystal structure: Microcrystalline (aphanitic); Cleavage: None; Specific gravity: 2.8–3.0
Formation & geological history
Formed from the rapid cooling of magnesium-rich and iron-rich lava at or very near the Earth's surface. This specific specimen has been rounded by fluvial processes (water erosion) in a river or stream environment over thousands of years.
Uses & applications
Used in construction as aggregate, road base, and railroad ballast. Smooth river-worn basalt is highly valued for landscaping, decorative gardens, and hot stone massage therapy. It is also used as raw material for stone wool insulation.
Geological facts
Basalt is the most common rock type in the Earth's crust and makes up most of the ocean floor. It is also found on the Moon and Mars. Due to its density and thermal properties, it can hold heat for long periods, making it ideal for therapeutic uses.
Field identification & locations
Identify in the field by its heavy weight (high density), dark color, and fine-grained texture with no visible individual crystals. It is commonly found in volcanic regions, along ancient lava flows, and in riverbeds. Magnetism may sometimes be present due to magnetite inclusions.
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Basalt (extrusive igneous rock) or Diabase (intrusive igneous rock - also known as Dolerite), largely composed of plagioclase feldspar, pyroxene (augite), and sometimes olivine and amphibole. Exact mineralogy would require thin section analysis.
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Magnetite
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Magnetite
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