Rock Identifier
Magnetite (lodestone), possibly meteoritic iron (Magnetite, Fe₃O₄; exact identification is uncertain from the image alone) — mineral
mineral

Magnetite (lodestone), possibly meteoritic iron

Magnetite, Fe₃O₄; exact identification is uncertain from the image alone

AI-generated identification · may be incorrect

Black to dark gray, metallic/submetallic luster, opaque, Mohs hardness 5.5–6.5, commonly massive rather than visibly crystalline, with uneven fracture and relatively high density (about 5.2 g/cm³). Strong attraction to a magnet would support magnetite;…

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Physical properties

Black to dark gray, metallic/submetallic luster, opaque, Mohs hardness 5.5–6.5, commonly massive rather than visibly crystalline, with uneven fracture and relatively high density (about 5.2 g/cm³). Strong attraction to a magnet would support magnetite; a metal file, nickel-rich composition, and unusually high density could indicate meteoritic iron.

Formation & geological history

Magnetite forms in igneous, metamorphic, and hydrothermal environments, while lodestone is naturally magnetized magnetite. The irregular, apparently melted or worked surface could also represent industrial slag or a processed specimen; geological age and origin cannot be established visually.

Uses & applications

Magnetite is an important iron ore, pigment, and dense aggregate; lodestones are collected for their magnetism. Meteorites have scientific and collector value.

Geological facts

The specimen appears black, heavy, and locally glossy, but the apparent cavity and smooth surfaces are not diagnostic and may reflect melting, cutting, or weathering.

Field identification & locations

Test magnetism, streak (magnetite gives a black streak), density, and nickel with professional analysis; avoid assuming meteorite status from appearance alone. Common sources include iron-ore deposits, beach placers, and volcanic terrains.