Rock Identifier
Yellow Ochre / Limonite (Limonite (Hydrated Iron(III) Oxide-Hydroxide, FeO(OH)·nH2O)) — mineral
mineral

Yellow Ochre / Limonite

Limonite (Hydrated Iron(III) Oxide-Hydroxide, FeO(OH)·nH2O)

Hardness: 4.0-5.5 (Mohs scale), Color: Yellow to brownish-yellow, Luster: Dull or earthy, Crystal Structure: Amorphous (microcrystalline), Cleavage: None, Specific Gravity: 2.7-4.3

Hardness
4
Identified More mineral

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Physical properties

Hardness: 4.0-5.5 (Mohs scale), Color: Yellow to brownish-yellow, Luster: Dull or earthy, Crystal Structure: Amorphous (microcrystalline), Cleavage: None, Specific Gravity: 2.7-4.3

Formation & geological history

Formed as a secondary material through the oxidation or chemical weathering of iron-rich minerals such as pyrite, magnetite, and siderite. Often found in hydrothermal veins or bog deposits.

Uses & applications

Major source of iron ore, historically used as a primary pigment (ochre) for paints and dyes. Currently used in industrial coloring and soil conditioners.

Geological facts

Yellow ochre is one of the oldest pigments used by humans, seen in cave paintings dating back over 30,000 years. It is chemically very similar to rust.

Field identification & locations

Identify by its distinctive mustard-yellow or 'ochre' streak on a porcelain plate and its earthy, non-crystalline appearance. Commonly found in weathered iron-bearing rocks or near marshes.