
mineral
Micrometeorite (Spherule)
Extraterrestrial Accretion Spherule
Hardness: 5-6 (Mohs); Color: Metallic black, brown, or translucent olive; Luster: Sub-metallic to vitreous; Structure: Spherical; Specific Gravity: 3.0-4.0.
- Hardness
- 5-6 (Mohs)
- Color
- Metallic black, brown, or translucent olive
- Luster
- Sub-metallic to vitreous
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Physical properties
Hardness: 5-6 (Mohs); Color: Metallic black, brown, or translucent olive; Luster: Sub-metallic to vitreous; Structure: Spherical; Specific Gravity: 3.0-4.0.
Formation & geological history
Formed when micrometeoroids enter Earth's atmosphere at high speeds (up to 72 km/s). Frictional heating causes the particle to melt and solidify into a sphere before hitting the surface.
Uses & applications
Scientific study to understand the chemical composition of the solar system and accretion history; highly valued by micrometeorite collectors.
Geological facts
Thousands of tons of this material fall to Earth every year. They are some of the oldest materials in our solar nebula. High-resolution microscopy and magnets are often used to find them.
Field identification & locations
Identify by spherical shape and magnetic response. Often found in accumulation zones like rooftops, deep-sea sediments, or Antarctic ice. Small size (sub-millimeter) requires magnification.
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