sedimentary

Banded Iron Formation (BIF) / Iron Ore

Banded Iron Formation (composed primarily of Hematite (Fe2O3) and Magnetite (Fe3O4) with Quartz/Chert)

AI-generated identification · may be incorrect

Hardness: 5-6 (Iron minerals) to 7 (Chert); Color: Reddish-brown, grey, black; Luster: Metallic to dull; Crystal structure: Microcrystalline; Cleavage: None/Conchoidal fracture; Specific Gravity: 4.5-5.3 (dense due to iron content).

Hardness: 5-6 (Iron minerals) to 7 (Chert)
Color: Reddish-brown, grey, black
Luster: Metallic to dull

Identified May 13, 2026More sedimentary →

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Physical properties

Formation & geological history

Formed in ancient oceans during the Precambrian eon (approx. 2.4 to 1.8 billion years ago) through the precipitation of iron from seawater as oxygen levels rose, creating alternating layers of iron oxides and silica.

Uses & applications

The primary global source of iron ore used in the production of steel for construction, infrastructure, and machinery. Also used as a decorative stone when high-grade (Tiger Iron).

Geological facts

These rocks provide the most significant geological record of the 'Great Oxygenation Event' in Earth's history. They are among the oldest sedimentary rocks on the planet.

Field identification & locations

Identified by distinct layering, heavy weight/high density, and reddish-brown streaks; many specimens are magnetic. Commonly found in Western Australia, Brazil, Lake Superior region, and South Africa.