Rock Identifier
Hematite Nodule (Hematite (Fe2O3)) — mineral
mineral

Hematite Nodule

Hematite (Fe2O3)

AI-generated identification · may be incorrect

Hardness of 5.5 to 6.5 on the Mohs scale, reddish-brown to steel-gray color, metallic to dull luster, and leaves a reddish-brown streak. It has no true cleavage and an uneven to conchoidal fracture.

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Physical properties

Hardness of 5.5 to 6.5 on the Mohs scale, reddish-brown to steel-gray color, metallic to dull luster, and leaves a reddish-brown streak. It has no true cleavage and an uneven to conchoidal fracture.

Formation & geological history

Formed through various processes including hydrothermal veins, sedimentary deposition, and weathering of iron-rich rocks. Common in desert environments and arid regions.

Uses & applications

Primary ore of iron, used in jewelry, as a pigment, and collected as a lapidary specimen.

Geological facts

Hematite has been used by humans as an artistic pigment for over 160,000 years, dating back to prehistoric cave paintings.

Field identification & locations

Identified easily by its characteristic reddish-brown streak on unglazed porcelain and high specific gravity. Plausible for the specified arid region in Iran which is rich in iron deposits.