Rock Identifier
Magnetite or Ironstone Nodule (Magnetite (Fe3O4) or Hematite-rich Sedimentary Nodule) — mineral
mineral

Magnetite or Ironstone Nodule

Magnetite (Fe3O4) or Hematite-rich Sedimentary Nodule

Hardness: 5.5-6.5; Color: Dark brown to black; Luster: Dull to metallic; Streak: Black or reddish-brown; Structure: Granular or massive; Magnetic properties often present.

Hardness
5
Color
Dark brown to black
Luster
Dull to metallic
Identified More mineral
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Physical properties

Hardness: 5.5-6.5; Color: Dark brown to black; Luster: Dull to metallic; Streak: Black or reddish-brown; Structure: Granular or massive; Magnetic properties often present.

Formation & geological history

Formed through the oxidation of iron-bearing minerals or as sedimentary concretions in iron-rich environments. Common in metamorphic belts and sedimentary iron formations.

Uses & applications

Major ore of iron; used in heavy industry, construction materials, and as magnetic media. Small nodules are mainly of interest to amateur geologists and collectors.

Geological facts

Magnetite is the most magnetic of all the naturally-occurring minerals on Earth. It was used by ancient navigators as a 'lodestone' to determine direction.

Field identification & locations

Identify by testing with a magnet (it will likely be attracted) and checking the streak color by rubbing it on unglazed porcelain. Commonly found in stream beds or eroded soil.