
mineral
Magnetite-rich Iron Ore
Magnetite (Fe3O4)
Hardness: 5.5-6.5; Color: Iron-black to brownish-black; Luster: Metallic to submetallic; Crystal structure: Isometric (octahedral); Cleavage: None (distinct parting in some specimens); Specific Gravity: 5.1-5.2
- Hardness
- 5
- Color
- Iron-black to brownish-black
- Luster
- Metallic to submetallic
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Physical properties
Hardness: 5.5-6.5; Color: Iron-black to brownish-black; Luster: Metallic to submetallic; Crystal structure: Isometric (octahedral); Cleavage: None (distinct parting in some specimens); Specific Gravity: 5.1-5.2
Formation & geological history
Formed in igneous or metamorphic environments through crystallization from magma or hydrothermal replacement. It is often found in banded iron formations (BIFs) and contact metamorphic deposits.
Uses & applications
Primary ore of iron used in the production of steel; also used in heavy media separation, as a pigment, and in magnetic recording media.
Geological facts
Magnetite is the most magnetic of all the naturally occurring minerals on Earth. Naturally magnetized pieces are known as lodestones and were used as the first magnetic compasses.
Field identification & locations
Identify in the field by its strong magnetic attraction, black streak, and high density. Commonly found in Kiruna (Sweden), Pilbara (Australia), and the Lake Superior region (USA).
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