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Ochre

Earth pigment of characteristic colour

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Hellocker- Pigment
Marco Almbauer · CC BY-SA 3.0

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Terminology

Ochre (sometimes "ocher" in American English,) is a natural clay earth pigment, consisting of a mixture of ferric oxide and varying amounts of clay and sand. The family of earth pigments known as ochre includes yellow ochre, red ochre, purple ochre, sienna, and umber. The major ingredient of all the ochres is iron(III) oxide-hydroxide, known as limonite, which gives them a yellow colour. A range of other minerals may also be included in the mixture:

The clays coloured with iron oxide derived during the extraction of tin and copper may also be known as ochre.

The term is also used for the colours produced by this pigment, especially a light brownish-yellow. The range of colours include:

  • Yellow ochre, FeO(OH)·nH
    2O - hydrated iron(III) oxyhydroxide (limonite) also called gold ochre.
  • Red ochre, Fe
    2O
    3·nH
    2O, takes its reddish colour from the mineral hematite, which is an iron oxide, reddish brown when hydrated.
  • Purple ochre is a rare variant identical to red ochre chemically but of a different hue caused by different light diffraction properties associated with a greater average particle size.
  • Brown ochre, also FeO(OH), (goethite), is a partly hydrated iron oxide. Similarly, lepidocrocite — γ-FeO(OH), a secondary mineral, a product of the oxidation of iron ore minerals, found in brown iron ores
  • Sienna contains both limonite and a small amount of manganese oxide (less than 5%), which makes it darker than ochre.
  • Umber pigments contain a larger proportion of manganese (5-20%), which makes them a dark brown.

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