Rock Identifier
Likely magnetite-rich iron ore (Magnetite (Fe₃O₄), possibly in a dense massive ironstone matrix) — mineral
mineral

Likely magnetite-rich iron ore

Magnetite (Fe₃O₄), possibly in a dense massive ironstone matrix

AI-generated identification · may be incorrect

Black to steel-gray, strongly metallic to submetallic luster, uneven fracture, and no obvious cleavage; Mohs hardness about 5.5–6.5, specific gravity approximately 5.2. The surface appears naturally granular and reflective, though lighting limits certainty.

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Physical properties

Black to steel-gray, strongly metallic to submetallic luster, uneven fracture, and no obvious cleavage; Mohs hardness about 5.5–6.5, specific gravity approximately 5.2. The surface appears naturally granular and reflective, though lighting limits certainty.

Formation & geological history

Magnetite forms in igneous, metamorphic, and hydrothermal environments, including banded iron formations and mafic or ultramafic rocks; many deposits are Precambrian (over 540 million years old).

Uses & applications

Used as an iron ore, dense aggregate, pigment, and source of magnetic media; attractive pieces are collected but are generally not jewelry-grade.

Geological facts

A hand magnet should attract it strongly, often more strongly than hematite. The specimen may be a massive magnetite ore rather than a single crystal.

Field identification & locations

Common worldwide, notably in Australia, Brazil, Sweden, South Africa, India, and the Lake Superior region of North America. Confirm with a strong magnet, streak test (black streak), and unusually high heft; avoid confusing it with slag or polished industrial iron.